Quick Key Facts
- Despite covering only around 25% of Earth’s land area, mountains host more than 85% of bird, mammal and amphibian species.
- Many of Earth’s rivers begin in mountains, and more than half of all people use freshwater from mountains every day.
- Six of the 20 plant varieties that feed most of the world’s population originate in mountains: barley, sorghum, tomatoes, apples, quinoa and potatoes.
- Mountain visits make up 15 to 20% of global tourism.
- Since 1950, mountains have been heating 25% to 50% faster than the global average.
- Even if global warming is limited to 1.5 degrees Celsius above pre-industrial levels, nearly all mountain glaciers will face considerable mass loss by 2100.
- The average Everest climber generates 18 pounds of waste, most of which stays on the mountain.
What Are Mountains and Why Should We Protect Them?
From the Alps and the Andes to Julie Andrews twirling in an alpine meadow in the opening scene of The Sound of Music, mountains have been a powerful force in human history and culture. They dominate our imaginations as they dominate our landscapes, towering over skyscrapers in cities from Tokyo to Seattle and forming islands from Hawaii to Iceland. A mountain, defined as a landmass significantly higher than its surroundings, comes in broadly four types: fold mountains, formed by the movements of tectonic plates; block mountains, created by rocks moving up and down; dome mountains, made from the movement of magma beneath the Earth’s crust and volcanoes.
While mountains are formed by geologic forces deep underground, they create space for unique ecosystems to form high above the Earth. Mountains’ harsh conditions and relative isolation have encouraged and sheltered varied biodiversity.
And what happens on mountains doesn’t stay on mountains. From crucial crops to glacial runoff, mountains have given many gifts to the human and non-human communities that live below them. Yet, society doesn’t treat mountains with the gratitude they deserve, threatening these majestic environments with the climate crisis, resource exploitation, pollution and overtourism. To preserve mountain ecosystems, it’s important for human communities to understand what mountains do for us and, in turn, what we can do for them.
What Are the Main Types of Mountain Ecosystems?
Mountain ecosystems vary wildly in climate and biodiversity. For example, mountains encompass the temperate European Alps and the Desert Mountains of Nevada to island-forming volcanoes like Hawaii’s Kīlauea and the world’s highest peaks in the Himalayas. The ecosystem changes within each individual mountain; this often depends on the altitude. For every 328 feet gained, the temperature falls by 0.9 to 1.1 Fahrenheit, and altitude conditions affect what species can survive and thrive in a particular spot. Similar plants and animals tend to thrive at similar altitudes (and latitudes moving north to south). These ecosystem bands are called life zones — below, we’ll detail out some of the most common.
Montane Forest
The first mountain life zone is the montane forest. Even if a mountain rises out of a lowland forest, the species in the montane forest tend to be distinct from those further below and will have more in common with trees that grow further north. In Europe, North America and temperate Asia, the trees in montane forests are typically conifers such as pines, mountain hemlocks and the unique larches of Washington State’s Cascades, with needles that turn yellow in the fall.
In the Southern Hemisphere’s temperate areas, montane forests are usually made up of one or two broadleaf species, such as eucalyptus in Australia, while in the tropics montane forests are usually evergreen rainforests. One unique tropical and subtropical type of montane forest is the cloud forest. These are evergreen rainforests whose moisture comes from clouds, which envelop the green in a constant mist. The clouds are first intercepted by the mountain slope and then filtered through the leaves. These forests, found in parts of Central and South America, Southeast Asia, Central and Southern Africa and Australia, are known for an abundance of plants like mosses, lichens and orchids that grow on other plants. The unique conditions that form cloud forests mean they’re home to many unique species, such as a carnivorous pitcher plant found in Borneo’s cloud forest called the Nepenthes hurrelliana.

Subalpine Zone
As altitude increases, climate conditions grow more extreme and trees have a harder time surviving. Eventually, they hit a point past which it is too cold, dry and low-oxygen for them to grow. This is called the tree line or timberline, and it typically occurs at the point on a mountain where temperatures during the warmest month average around 50 degrees Fahrenheit. The area immediately around the tree line is a transition area between tree-dominated and tree-free ecosystems. This is called the subalpine zone.
The trees that grow in the subalpine zone are often shorter than those below it. Some will grow in the shadow of rocks and won’t grow higher than the rock’s protection. Others will grow out instead of up. These low, wind-twisted trees are called krummholz, the German word for “crooked wood.” Between the krummholz are subalpine meadows where many species of wildflowers flourish, depending on the region. In temperate ecosystems, common flowers are heather, daisies, lupins and pasqueflowers.
Alpine Tundra and Grassland
Above the tree line, conditions grow even harsher, which limits what can grow. The plants that survive grow low to the ground year-round and include grasses, sedges, forbs and lichens. Grasses grow most frequently in alpine meadows, which are created when weather conditions have eroded rocks sufficiently to create soil. Alpine flowers have evolved to have hair on stems and leaves that protect them from the wind. One example is the Edelweiss, or Leontopodium nivale, which grows in the Alps and Carpatihians, a national symbol for several countries in the region. Other alpine flowers have red pigment to help turn the sun’s rays into heat or blue to protect against ultraviolet radiation, such as the Clusius’s gentian in the Swiss Alps.
Many alpine ecosystems around the world will have similar types of plants, including heather, gentians, plantains and buttercups. Tropical alpine regions in the Andes, the Himalayas, East Africa and Pacific islands feature a unique type of plant, a large herb with a rosette structure that can grow to be over 10 feet tall. WWF considers montane grasslands and shrublands to be their own biome. These ecosystems occur all over the world from the Páramo in the Northern Andes to the steppes of the Tibetan plateau. Even higher up, some mountains see ice and snow year-round, conditions that are inhospitable to most life. However, some organisms still find a way, such as ice worms and red algae in the North Cascades or the microbes that have been discovered beneath mountain glaciers.

What Are the Benefits of Mountains?
Mountains have a myriad of benefits, from housing ample biodiversity and providing freshwater to being recreational destinations where people can hike and ski.
Habitats and Biodiversity
Despite only covering around 25% of Earth’s land area, mountains are essential havens for biodiversity, hosting more than 85% of birds, mammals and amphibians and one-third of terrestrial species. They also include almost 25% of the world’s forests. The tropical Andes in South America are home to 45,000 plant species, while the mountains of New Guinea alone host 20,000 plant and animal species. Unique animals that shelter on mountains include iconic species like bighorn sheep, red pandas, orangutans, snow leopards, Rocky Mountain goats, the Himalayan tahr and the California and Andean condors.
The biodiversity importance of mountains comes in part from their elevation and their relative isolation from the landscape below. Their altitude and cooler temperatures allowed them to act as a refuge for cold-weather species as planetary temperatures warmed following the last Ice Age. In more recent history, they provide a haven for species pushed out of the lowlands by human activity. At the same time, the contained environments of mountains enable species to evolve and diverge relatively quickly, so that different but related species can survive on nearby mountain peaks, boosting overall biodiversity. Mountains can also support the biodiversity below them. For example, snowmelt from Mount Kilimanjaro waters the swamps of Amboseli National Park, which shelters 420 bird species and 50 large mammal species.
Water
Mountains are essential to the global freshwater supply, so much so that they’ve known as the “world’s water towers.” Mountains store water in glaciers, snowpacks, lakes and reservoirs that flow downhill at increased rates during warmer weather. Most of the Earth’s largest rivers begin in mountains, and more than half of all people use fresh water from mountains every day for drinking, sanitation, agriculture, electricity, industry, transportation, recreation and fisheries.
Certain ranges are especially important as regional water sources. Scientists have identified 78 mountain “water towers” that are especially vital, providing water to 1.9 billion people. The greatest number of people are dependent on the Indus river system coming out of the Himalayas in Asia. More than 200 million people in the region and 1.3 billion people downstream rely on water from the Hindu Kush-Himalayan mountain region alone, which is sometimes called the world’s “Third Pole” for its abundance of mountain glaciers. Other important “water tower” mountains are the European Alps, the U.S. Rockies and the southern Andes in South America. Cities that rely on mountain water include Tokyo, Rio de Janeiro, New York, Nairobi and Melbourne.
Food and Flowers
Because their harsher conditions put stress on plants, mountain soil is less nutrient-rich overall than lowland soil. Therefore, mountains aren’t used for agriculture on a large scale. That said, several important food crops and beloved garden flowers originated on mountains. These include six of the 20 plant varieties that feed most of the world’s population: barley, sorghum, tomatoes, apples, quinoa and potatoes. Potatoes, for example, were first domesticated in the Andes around 8,000 years ago. Gardens would also be noticeably less bright without mountains, as many popular flowers originated in mountains. More than 60% of wild tulip species evolved in the mountains of Central Asia.
Culture
Currently, between 0.3 billion and 2.3 billion people call mountains home. Communities who have lived on mountains for centuries have developed their cultures based on their alpine lifestyles.
The Sherpas live in the most mountainous part of the Tibetan and Nepalese Himalayas. They’ve become so well known for their mountaineering prowess that the term “sherpa” is now used for any mountain guide in the region, regardless of ethnicity. Switzerland’s iconic yodeling singing style originated from shepherds calling to each other across the Alps. In fact, most mountain ranges are home to Indigenous peoples and local communities who depend on them for sustenance and identity.
Many of these communities have developed unique Indigenous knowledge systems, such as languages, traditions and ways to make use of the land. Many cultures also consider certain mountains and glaciers sacred. Mount Kailas in Tibet is honored by Buddhism, Hinduism, Jainism, Sikhism and Bon. Other mountains that hold spiritual significance to different groups include Mount Everest, Mount Fuji, Mount Ararat, Mauna Kea, the Mount Olympus (of Greek mythology) and Mount Shasta, where the Winnemem Wintu people of California believe all of life bubbled up from a mountain spring.

Recreation
Mountains provide ample opportunities for recreation in nature, such as mountain and rock climbing, hiking, mountain biking, backpacking, camping, downhill and cross-country skiing, snowboarding and snowshoeing. They also host sites of cultural or historical significance, such as the Incan ruins of Machu Picchu in Peru, which draws millions of visitors annually. In fact, mountain visits make up 15 to 20% of global tourism. Mountain and snow tourism generated at least $4.9 billion in 2023, which is expected to grow to $8 billion by 2033.

Main Threats to Mountains
When you see craggy peaks towering above the lowlands or spewing ash and lava into the sky, mountains may seem invincible to the whims of humans. Yet their size and power can’t protect mountain ecosystems from the same environmental pressures that human activiy is placing on the rest of the world.
Climate Threats
Scientists have warned that climate change (driven by the burning of fossil fuels), is the greatest threat to mountain ecosystems.
Climate Shift
For every degree that lowlands warm, mountains warm on average 1.8 degrees Celsius. And since 1950, mountains have been heating 25% to 50% faster than the global average. This speed of warming can alter ecosystems faster than plants, animals and humans can adapt, increasing the risk that diseases or invasive species will rise to new mountain life zones and harm native species. The shifting of mountain life zones could threaten unique alpine species with mass extinction.
This rapid warming also threatens the snow and ice that shape alpine life, culture and recreation. One study found that the U.S. ski industry lost $5 billion between 2000 and 2019 due to a lack of snow and the cost of making artificial snow to compensate. Another calculated that 1 in 8 current ski areas wouldn’t get any natural snow cover by 2100. This would threaten local economies that depend on tourism as well as mountain biodiversity, as ski slopes are constructed in higher, more remote areas to chase the remaining snow, shrinking the undisturbed habitats home to mountain life.
Glacier Melt
Perhaps the climate mountain threat that could harm the largest amount of people is the melting of mountain glaciers. This threatens mountains’ status as the world’s water towers, putting the freshwater and energy of over a billion people at risk.
Non-polar glaciers lost around 267 metric gigatons of mass per year between 2000 and 2019 and doubled their rate of thinning during the same time period. A 2023 study found that even if warming is limited to 1.5 degrees Celsius, nearly half of all glaciers will melt by 2100. If warming is allowed to reach 2.7 degrees Celsius, 68% would melt. If it reached four degrees, 83% would disappear. Beyond the impact on mountain or mountain-reliant communities, the melting of these glaciers would also contribute to sea-level rise, pushing up water levels by just under 4 inches in the 1.5 degrees scenario and 4.5 inches in the 2.7 degrees of warming — submerging an area where more than 10 million currently live.
Mountain Disasters
Warmer temperatures and glacial melt also increase the risk of mountain disasters such as landslides, rockslides and floods. When glaciers retreat and mountain permafrost melts, this can cause flooding, as there is more water running down the mountain more quickly. It can also destabilize the ground, increasing the risk of land movements like landslides, rockslides and avalanches in warm or thick snow. The climate crisis has also increased the risk of a specific type of flood known as a glacial lake outburst flood. These floods occur when glacial meltwater pools in lakes that are then destabilized by an earthquake, rain storm or dam breach, sending massive amounts of water down the hillside. The number, volume and area of these lakes have increased by 50% since 1990, and 15 million people are now threatened by these types of floods, especially in the Himalayas and the Andes.
Other Threats
The high biodiversity of mountain ecosystems also makes them vulnerable to human threats. Because mountain species have evolved to succeed in such unique environments, they can be easily harmed if that unique ecosystem is threatened. For example, the Taita thrush is only found in the Taita hills of Kenya; it can’t survive in the drier grasslands below.
Habitat / Biodiversity Loss
Human activity can threaten mountain ecosystems directly through development, deforestation and the introduction of invasive or pest species. When a larger number of humans move up into the mountains to live or farm, this can displace native plants and animals and increase human-wildlife conflict when the wild mountain species eat crops or livestock. Poachers also target lower mountain mammals.
In the past, mountain forests haven’t experienced aggressive deforestation like lowlands have. However, this is starting to change. Between 2000 and 2018, humans cleared 78 million hectares of montane forest. The main causes of this deforestation were commercial logging, tree clearing for agriculture and wildfires. The most deforested mountain areas tended to coincide with tropical biodiversity hotspots.
One example of this trend is Southeast Asia, which is home to around half of all tropical montane forests. There, upland forest loss has accelerated in the 2010s, accounting for 42% of the region’s total as of 2019. Mountain forest loss can also increase the risk of flooding and erosion, worsening water quality and affecting native flora and fauna. Species that might need to shift their range to accommodate rising temperatures have less habitat to work with. Southeast Asia’s mountain forests are also especially adept at storing carbon compared with lowland forests, so removing them makes it harder to keep both local and global temperatures lower.
Pollution
The main sources of pollution for mountains are human activities like logging, mining, logging, agriculture, grazing and recreation, as well as the transport of smaller pollutants through the atmosphere. Air pollution from urban or industrial centers can travel to mountains, where it not only worsens air quality but also enters plant tissue, soil and water. This pollution has harmed forests in the Carpathian mountains and brought smog to Great Smoky Mountains National Park, where at one point ozone had harmed almost half of the black cherry trees and 79% of milkweed plants sampled. Microplastics have also been found high in mountain ranges, from Mount Everest to the Alps.
Overtourism
While mountain recreation can provide an economic boost to local communities and offer visitors a chance to learn about and appreciate mountains, it has a downside. Sometimes, mountain tourists are not as respectful as they should be or tours are not designed to account for the impact of visitors to vulnerable ecosystems.
Increased visitors can bring more construction of tourist infrastructure like ski lodges or cabins, increased vehicle traffic that emits air pollution, noise and light pollution that disturbs animals, problems with proper waste disposal, disturbance of mountain wildlife and negative encounters with local communities.
One example of overtourism gone wrong is Mount Everest, the world’s tallest mountain from sea level and a major climbing destination. So much waste has accumulated on Everest that it has been called the “world’s highest garbage dump.” Around 100,000 people visit Everest’s Sagarmatha National Park every year, and around 600 try to summit the mountain every climbing season. The average climber generates 18 pounds of waste, most of which stays on the mountain. In addition to larger debris like abandoned tents, oxygen canisters and even dead bodies, climbers also leave behind human waste. With increased melt and runoff from climate change, some of this waste has begun to flow into the local water supply, putting people downstream at risk from dangerous diseases like cholera and hepatitis A.
How to Protect Mountains
Humans have the power to harm mountain ecosystems, but we also have the power to protect them. The decisions we make as citizens, consumers, policymakers and tourists can have a positive impact on these magical environments.
Protecting Mountains From Climate Change
As previously discussed, climate change is one of the biggest threats to mountains and glaciers.
Mitigation
The most important way to protect mountains from the climate crisis is the same as the most important way to protect the entire Earth: We must phase out fossil fuels as rapidly as possible. This means both preventing development of new fossil fuel deposits, replacing oil, gas and coal with renewable sources of energy like wind and solar and transitioning from gas-powered cars to electric vehicles while improving public transportation options. In its most recent assessment, the Intergovernmental Panel on Climate Change recommends nearly halving greenhouse gas emissions by 2030 and reaching net zero by 2050 in order to limit global warming to 1.5 degrees Celsius above pre-industrial levels.
The second main driver of the climate crisis is the destruction of natural carbon sinks through deforestation and other forms of land-use change. This means that protecting mountain habitats has a double benefit for mountains: It preserves an individual ecosystem from immediate disturbance and it lowers the impacts of climate change on all mountains.
Adaptation
Even if world leaders succeed in winding down the use of fossil fuels and limiting global warming to 1.5 degrees Celsius of warming — something that seems increasingly unlikely — mountain communities will need to adjust to the climate impacts they’re already experiencing and the ones that are projected to continue, such as the loss of nearly half of mountain glaciers by 2100.
Some are already taking action. Resort employees on Switzerland’s Mount Titlis have started covering the mountain’s glacier with protective polyester fleece during the summer. Venezuela is restoring wetlands to deal with water shortages. And in the Hindu Kush Himalaya region of Pakistan, communities are working to establish an early-warning system for more frequent floods. The Adaptation at Altitude program seeks to help mountain communities become more resilient to climate change by researching effective solutions and sharing them across alpine regions.
Unfortunately, the IPCC found that current mountain adaptations are not fast, expansive or substantial enough to respond to a high level of climate risks. Policymakers can boost the adaptive ambition of mountain regions by fostering international collaboration. They can developing holistic projects that consider all the needs of mountain communities, support more research and data gathering and making sure mountain communities have the funds they need.
Protecting Mountains From Other Threats
Beyond climate change, there are other issues that can harm mountains.
Exploitation and Deforestation
Governments, corporations and individuals can take steps to protect mountain ecosystems from exploitation. Research into mountain deforestation found that deforestation was less likely to occur in protected areas, so conserving mountain ecosystems — and safeguarding the land rights of any Indigenous communities that steward them — is one immediate way to prevent further habitat and biodiversity loss.
Scientists say these protected areas should be large enough to give species space to move. Governments can also regulate extractive industries and support ecological restoration and agroforestry efforts. They can plan dams and other infrastructure in such a way that won’t disturb waterflow or wildlife. Restoration or reforestation projects should replant a variety of native species rather than single tree species in monoculture plantations.The international community could also negotiate treaties to specifically protect mountain ecosystems.
Tourism companies can follow best-practices to make sure that they are being mindful of the limits of mountain ecosystems and the rights of local communities. Larger food or lumber corporations can make sure that their supply chains are deforestation-free. Consumers can choose to support companies that respect mountain ecosystems and avoid those that don’t.
Responsible Climbing and Tourism
One of the most important ways individuals can protect mountains is to behave responsibly when they visit them. This means following the principle of “leave no trace” and taking anything you bring to a mountain with you when you leave. Other things you can do are travel during off-peak season or to less popular destinations, rely on non-fossil fuel transport when possible, support sustainable tourism companies, be respectful of Indigenous or local communities you encounter, buy second-hand gear or share equipment with others and spread awareness of these best practices to other hikers. If you are lucky enough to trek Mount Everest, make sure to offset your climb by bringing your waste back down with you.
Takeaway
“The mountains are issuing a distress call,” said United Nations Secretary-General António Guterres at a 2023 United Nations climate change conference.
That distress call comes in the form of melting glaciers, sudden floods, snowless ski slopes and falling forests. If human societies choose to ignore that call, they could usher in a future in which mountains are unrecognizable, as glaciers, snowpacks and entire niches of species disappear. However, if we can learn to work with mountains to stop exploitation, the outlook for mountains might be brighter.

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Green Living
Methane 101: Understanding the Second Most Important Greenhouse Gas
By Olivia Rosane and Cristen Hemingway Jaynes
Quick Key Facts
- Methane is the second most important greenhouse gas after carbon dioxide and is responsible for around one-third of current global heating.
- Atmospheric methane concentrations have increased by 256 percent since pre-industrial times.
- Methane is a more powerful greenhouse gas than carbon dioxide but lasts for far less time in the atmosphere; over a 20-year period, methane traps 86 times more heat per unit of mass than CO2.
- Around 60 percent of methane emissions come from human-caused sources and 40 percent come from natural sources.
- Ninety percent of human-caused emissions come from three sources: fossil fuels, agriculture and waste storage.
- Currently existing strategies, if adopted, would be enough to curb methane emissions from these three sources by 45 percent by 2030.
- It is possible to cut methane emissions from oil and gas operations by 70 percent with existing technologies and methods and by 40 percent at no cost.
- Studies have shown that adding seaweed supplements to the diets of cattle can decrease their methane emissions by 82 percent for feedlot cattle, more than 50 percent for dairy cows and 42 percent for grazing cattle without harming the animals.
- As of 2023, only 13 percent of all methane emissions were covered by any sort of emissions-reduction policy.
- If everyone in the European Union limited their meat and dairy consumption by 34 percent, they would prevent six million metric tons of methane emissions per year.
What Is Methane?
What has no color or smell and is found in wetlands, cow burps and your basement furnace? The answer is methane — a powerful greenhouse gas that is the second most important contributor to the climate crisis after carbon dioxide (CO2). It is the primary component of natural gas, which currently generates around 25 percent of the world’s electricity.

Methane is a hydrocarbon composed of four hydrogen atoms bonded to a carbon atom. It is abundant in nature and can be formed by both geological and biological processes. Geologically, methane is typically created when heat and pressure are applied to decomposing plant and animal matter over millions of years. This is the source of most natural gas. Methane can also form deep underground without any organic matter through other processes. Biologically, methane is generated through something called methanogenesis, when certain underwater microorganisms called archaea produce methane as part of their oxygen-free respiration process. This is how methane is generated above ground, such as in wetlands or in the digestive tracts of termites and cows.
How Is Methane Measured?

Methane is measured via two main methods: bottom up and top down. These methods work almost exactly as they sound. Bottom-up approaches begin on the ground with a localized source of methane and expand outward. These assessments can either be based on direct measurements of a given facility’s methane emissions or by estimations based on general knowledge about the emitting animal or equipment. For example, to estimate the methane produced by a region or country’s beef or dairy sector, a bottom-up approach could multiply the methane emitted per cow by the number of cows being raised. A similar approach could be used to calculate the methane released by a county’s natural gas facilities or a region’s oil drilling operations.
Top down approaches often literally start in the sky with measurements of atmospheric methane, usually via airplane, high-altitude platforms or, increasingly, satellites. This data can then be combined with knowledge of where there are methane sources and sinks and used to create models of methane emissions.

Satellite image of methane emissions from a landfill in Kyrgyzstan on Feb. 4, 2021. GHGSat
As satellite technology improves, it is detecting super-emitting incidents that are not reflected in bottom-up approaches. For example, if a gas company assesses its methane emissions by multiplying the standard leak rate of a piece of equipment by the number of pieces of that equipment it uses, it will miss the five percent of extraordinary leaks that are responsible for more than half of all gas-industry leak emissions. Overall, direct measurements — whether from the ground or the air — are important for accurately measuring fossil fuel methane emissions in particular. One study found that direct measurements of U.S. oil and gas methane emissions were 60% higher than U.S. Environmental Protection Agency estimates. In general, improving methane measurements is essential for understanding and therefore controlling its emissions.
How Does Methane Contribute to the Climate Crisis?
Methane is a greenhouse gas, which means that, when it enters the atmosphere, it absorbs heat energy emitted from the planet and redirects it back toward the ground. There are natural methane sinks — namely soil and the troposphere, where methane is broken down into carbon dioxide and water vapor. These sinks are able to counteract naturally occurring methane emissions so that the gas does not build up in the atmosphere. However, human activities since the start of the industrial revolution — particularly the burning of fossil fuels, more intensive forms of agriculture and waste storage — have raised the concentration of methane in the atmosphere faster than natural sinks can absorb it.
As of 2023, the most recent year for which data is available, atmospheric methane concentration had soared by 265 percent to 1,934 ppb compared with pre-industrial levels. Around 60 percent of that methane was emitted due to human activities. That methane has contributed to around one-third of current global heating, second to CO2 at around two-thirds. If nothing is done to reduce methane emissions, they are projected to rise by 13 percent between 2020 and 2030.
Controlling methane emissions is essential for addressing the climate crisis because methane is both more potent than CO2 and also lasts for a shorter period of time in the atmosphere, approximately 12 years compared with hundreds. Over a 20-year period, methane traps 86 times more heat per unit of mass than CO2, which falls to 28 times more over 100 years. The combination of methane’s potency and relatively short atmospheric lifespan means that reducing methane emissions delivers a powerful bang for one’s buck in terms of rapidly curbing greenhouse gasses and stabilizing global temperatures. In fact, the Global Methane Assessment concluded that curbing methane “is very likely the strategy with the greatest potential to decrease warming over the next 20 years.” The Intergovernmental Panel on Climate Change (IPCC) has calculated that methane emissions must be reduced by around 34 percent by 2030 when compared with 2019 levels in order to limit global heating to 1.5 degrees Celsius above pre-industrial levels.
What Are the Main Sources of Methane?
Methane comes from both human and natural sources, with human-caused emissions responsible for around 60 percent of atmospheric methane and natural sources around 40 percent. More than 90 percent of current human-caused methane emissions come from three sources: agriculture, fossil fuels and waste storage. The burning of biomass and the use of biofuels also emit methane but are less important, as they are responsible for around five percent of emissions. Wetlands and freshwater are the leading source of natural methane emissions, followed by geological sources such as gas-oil seeps and volcanoes, termites, oceans, wild animals and permafrost. In addition, there are natural sources of methane that could play a larger role in the future as the climate crisis triggers various feedback loops.
Agriculture

Around 40 percent of human-caused methane emissions come from agriculture. The vast majority of these emissions are from livestock, which alone generate around 32 percent of human-caused methane emissions. This is primarily from enteric fermentation, which is how ruminant animals like cows, sheep and goats digest their food. Microbes in these animals’ digestive systems break down nutrients and produce methane as a byproduct. When it comes to methane emissions, cows raised for meat or milk are the primary contributors. Another way that livestock agriculture can generate methane is through the storage of manure, particularly that of pigs and cows. As meat consumption increases, these emissions are projected to rise by six million metric per year by 2030.
A second important agricultural contribution to human-caused methane emissions is the cultivation of rice at eight percent. Rice is grown in flooded patties, an environment that encourages the growth of methane-producing microbes. Finally, around one percent of human-caused methane emissions are caused by the burning of agricultural waste.
Fossil Fuels
The extraction and burning of fossil fuels contribute around 35 percent of human-caused methane emissions. Primarily, this occurs through the extraction, transport and use of oil and gas, at 23 percent of human-caused emissions. Methane is typically released during venting, when unwanted gas is released into the atmosphere during the extraction process, as well as through accidental leaks from extraction to transport to use. Emissions from oil and gas are expected to increase by 10 million metric tons per year by 2030, in particular because of the use of natural gas.
Around 12 percent of human-caused methane emissions are released during the process of mining coal, or from leaks from abandoned coal mines. Methane naturally occurs along coal seams, and can be released in several ways during the mining process: through seepage when the coal is exposed to the surface, through drainage systems, through ventilation systems to reduce methane buildup in a mine for safety reasons and from the coal itself as it is removed from the mine. Underground mines tend to emit more methane than surface mines, at 70 percent of mine emissions.

Certain fossil fuel projects emit massive amounts of methane at once, usually due to leaks or venting. These are called “super-emitters” and are detectable through satellite imaging. In 2022, researchers detected more than 1,005 human-caused super-emitter incidents — 559 at oil and gas fields and 105 at coal mines. The worst, in Turkmenistan, spewed 427 metric tons of methane per hour, the equivalent of the hourly emissions of France. As methane emissions increased in the 2010s, experts think that fossil fuel activities contributed as much as agriculture and waste storage combined.
Landfills and Waste
Around 20 percent of human-caused methane emissions come from landfills and waste management systems. This is because microbes present in wastewater treatment facilities and landfills release methane as they decompose the waste. This can generate lots of methane at once: Of the 1,005 super-emitter events identified by researchers in 2022, 340 were from waste sites.
Because of population growth and projected development in poorer countries, emissions from waste are expected to grow faster than from any other human-caused methane source at 13 million metric tons per year by 2030. The amount of human-disposed solid waste overall is expected to rise by 73 percent by 2050.

Wetlands
Wetlands are the predominant source of natural methane emissions, accounting for around one-third of total methane emissions. This is because wetlands — which cover around six percent of the Earth’s land area — are defined by having their soils saturated with water for all or part of the year. This creates a wet, oxygen-poor environment that creates ideal conditions for the archaea responsible for methanogenesis.
While wetlands would produce methane no matter what humans do, the climate crisis has led to an increase in wetland methane emissions in recent years due to temperature increases and changing rainfall patterns. This is known as the “wetland methane feedback.” Between 2000 and 2020, wetland methane emissions increased by 1.2 to 1.4 million metric tons per year, which is a higher rate than anticipated by the most pessimistic emissions scenarios. Scientists noted that these emissions saw “exceptional growth” in 2020 to 2021 in particular. The researchers traced this increase to two sources: tropical wetlands and permafrost wetlands.
Tropical wetlands are expanding their area due to climate-fueled changes in rainfall patterns and were the major driver of increased wetland methane emissions in the early 21st century. Permafrost wetlands are located in the Arctic and, as the name suggests, are partially frozen in addition to being waterlogged. When warmer temperatures cause permafrost to melt, they also unfreeze the microbes that release methane. Arctic wetlands have also expanded by 25 percent during the summer due to a rise in precipitation.
Oceans
The ocean is responsible for one to 13 percent of natural methane emissions through various mechanisms including geological marine seepage; emissions from ocean sediments or melting underwater permafrost; emissions near coastal areas where groundwater enters the sea; and the destabilization of methane hydrates, which are ice-like formations of methane and water on the seafloor. The largest concentration of methane on Earth is stored in these hydrates, and there are concerns that, as the climate crisis causes oceans to warm, these deposits might melt and release massive amounts of methane into the atmosphere. However, there is no evidence that any methane from these hydrates is currently reaching the atmosphere.
Positive Climate Feedback Loops
A positive feedback loop occurs when a change to a given system triggers other changes that amplify that initial change. In the case of the climate emergency, a positive feedback loop occurs when the impacts of global heating interact with Earth’s systems in ways that trigger more warming. When these changes pass a certain threshold, it can alter the system in dramatic and irreversible ways. This is called a climate tipping point.
Methane is involved in several positive feedback loops, of which the wetland methane feedback is just one example. Another related example is the thawing of the Arctic permafrost, frozen soils on land as well as beneath the Arctic Ocean. The material that is frozen beneath the permafrost contains plant and animal matter, as well as microbes that would produce methane if they thawed out. The permafrost beneath the ocean contains methane hydrates. This means that the Arctic currently contains 2.5 times more carbon underground than exists in the atmosphere. Thawing the permafrost would release all or some of that carbon, triggering a major tipping point. This process has already begun, with Arctic and Boreal methane emissions increasing by 9 percent since 2002. Scientists don’t know exactly how much methane the melting permafrost might ultimately release, but the region is currently on pace to release the greenhouse gas emissions of a major industrialized nation if nothing is done to reduce warming.
Another positive climate feedback loop involving methane is the increase in the frequency, severity and size of wildfires. A warmer climate makes the hot, dry conditions that fuel wildfires more likely, and these fires in turn release carbon dioxide and methane into the atmosphere as they burn, fueling more warming. Larger fires also tend to release more methane. One study found that California’s record-breaking 2020 wildfire season contributed almost 14 percent of the state’s total methane emissions for the year.
Methane and the ‘Bridge Fuel’ Myth
Another reason methane emissions might spike in the future is the expansion of gas production, including an increase in exports of liquefied natural gas (LNG). The development and spread of fracking in the U.S., Canada and Australia in particular has made gas much more abundant and set off a construction boom in infrastructure to export and import the fuel. The U.S. has massively increased its LNG exports since it lifted a ban on them in 2016, becoming the No. 1 natural gas exporter in the world by 2022. These exports doubled between 2019 and 2021 and will double again in four years if they continue.
Advocates of natural gas have argued that it is a “bridge fuel” from coal to more renewable sources of energy. This is because when burned for energy, coal emits twice as much carbon dioxide per kilowatt-hour as natural gas. In the U.S., direct power plant emissions decreased by almost 40 percent in the first decades of the 21st century, as gas overtook coal as the country’s leading electricity fuel source. Proponents of exporting U.S. LNG argue that it would similarly displace coal use in Europe and Asia. However, this ignores the methane that leaks during the process of extracting and transporting LNG. If only 0.2 percent of methane leaks, it makes LNG as climate-warming as coal, and new data, including satellite imagery, suggests that the amount of methane leaks have been vastly underestimated. A 2023 study calculated that, when methane leaks are taken into account, LNG has a 33% greater global warming potential over 20 years than coal. Further, the Department of Energy recently concluded that LNG exports are more likely to replace renewable energy sources than coal.
This new understanding comes as more gas fields and LNG export and import terminals are being planned. A 2022 analysis found that there are 55 “methane bomb” gas fields whose future methane leaks would equal 30 years of U.S. greenhouse gas emissions. The current and proposed construction of LNG export terminals in the U.S., meanwhile, would cancel out any climate progress the nation has made, keeping its greenhouse gas emissions frozen at 2005 levels. As U.S. climate campaigner Bill McKibben warned, “If the LNG build-out continues — here and in Canada and Australia — its sheer size will overwhelm our efforts to rein in global warming.”
What Are Other Benefits to Reducing Methane Emissions?
While stopping the acceleration of the climate crisis is a major argument for reducing methane emissions, these emissions don’t just heat the atmosphere. They also contribute to ground-level ozone, which forms as methane reacts to the atmosphere. Ozone at ground level is a major public health and environmental hazard because it damages human lung tissue, triggering respiratory ailments, and harms plants including agricultural crops. Currently, methane-generated ozone causes about half a million extra deaths per year. However, every million metric tons of methane emissions avoided would also prevent 1,430 yearly deaths from respiratory and heart diseases; 4,000 asthma-related emergencies and 90 hospitalizations per year; and annual losses of 145,000 metric tons of wheat, soybeans, maize and rice.
What Can Be Done to Reduce Methane Emissions?
There are many ways to reduce methane emissions that range from large-scale transformations of energy and food systems to smaller technical fixes. Most likely a combination of methods will be necessary to control methane emissions to reduce global heating and ozone pollution. However, currently existing methods, if adopted, would be enough to curb methane emissions from the three main human-caused sources — fossil fuels, agriculture and waste — by 45% by 2030, in line with the IPCC’s pathway to 1.5 degrees.
From Agriculture
There are two main ways to reduce the amount of methane produced by the food system. The first is to transform the food system altogether by reducing meat and dairy production. This can be done in part by reducing food waste, as 30 to 40 percent of all food produced is lost and does not make it to a person’s stomach. According to one calculation, the waste of ruminant and rice products is responsible for around 50 million metric tons of methane per year, and reducing it could cut those emissions by around 20 million metric tons. Another way is to shift toward more healthy, sustainable or plant-based diets, including by reducing overall consumption in wealthier countries. According to the IPCC, doing so would reduce greenhouse gas emissions overall by 5.3 to 20.2 gigatons of carbon-dioxide equivalent by 2050. Potential emissions reductions from dietary shifts run from 0.7 to eight gigatons of carbon dioxide equivalent per year by 2050, under scenarios ranging from half of the planet adopting a “healthy” diet that includes less than six grams of animal protein per day to a global embrace of vegetarianism.
The second main strategy for reducing methane emissions from agriculture is to make changes to existing production so that it releases less methane. One way to do this is to increase the efficiency of animal agriculture so that more meat or milk is produced per animal, especially in poorer countries. This can be done without sacrificing animal welfare by feeding animals better diets, including highly digestible feed; improving animal health overall; and breeding. Another solution is to add enteric methane inhibitors to the diets of ruminants, which prevent methane production in their guts. Promising examples are the chemical 3-NOP and seaweed. Studies have shown that adding seaweed supplements to the diets of cattle can decrease their methane emissions by 82 percent for feedlot cattle, more than 50 percent for dairy cows and 42 percent for grazing cattle without harming the animals in any way. Researchers are also working to breed ruminants who produce less methane and to develop a vaccine that would limit gut methane production.
Another major source of agricultural methane that can be targeted for reduction is manure storage. Solutions include reducing the amount of time manure is stored; covering tanks holding semi-solid waste; separating liquid and solid manure; and adding acid to manure storage facilities, which inhibits the growth of methane-producing microbes. Another solution that has been adopted in recent years is the use of manure digesters, which turn manure into biogas, reducing manure’s methane emissions and providing a non-fossil form of energy. However, there are emerging concerns that methane leaks from these machines may undermine their impact.
Finally, emissions from rice can be curbed by various methods. One strategy is to grow either higher yield or lower-methane varieties of rice, which reduce the amount of methane emitted per kilogram. Planting lower-methane rice could cut emissions by 22 to 51 percent. Another option is to change how rice is grown by using Alternative Wetting and Drying. Instead of keeping rice paddies flooded, this method involves letting them dry out completely before flooding again and can decrease emissions by 40 to 45 percent. Finally, adding phosphogypsum and sulphate to rice fields can decrease microbial methane production.
From Fossil Fuels
The No. 1 way to reduce methane emissions from fossil fuels is to phase out their use entirely as soon as possible while rapidly transitioning to renewable forms of energy that do not emit methane and in particular to halt the buildout of LNG infrastructure. However, there are also ways to reduce the methane emissions from fossil fuel infrastructure still in use, and in fact reducing methane emissions from ongoing oil and gas operations is considered the strategy with the most short-term potential for significant methane cuts.
According to the International Energy Agency (IEA), it is possible to slash the oil and gas sector’s methane emissions by 70% with existing technologies and methods and by 40% at no cost. These methods include leak detection and repair, installing devices to detect methane and phasing out equipment that releases methane when used. For coal, it is more difficult to reduce emissions while still mining and burning coal, but there are strategies such as requiring new mines to use degasification wells and drainage boreholes to capture methane and capturing and reusing methane in existing mines. It is also possible to avoid methane emissions from equipment no longer in use by capping abandoned gas wells and flooding retired mines.
From Landfills and Waste
Ideally, the best way to reduce methane waste from landfills would be to move toward a zero-waste circular economy that reuses all material throughputs. Specific strategies toward this goal include reducing food waste, keeping organic waste out of landfills and diverting it toward composting systems, capturing methane emissions from landfills and covering landfills with soil containing organisms that can break down methane.
Reducing methane emissions from wastewater can mostly be achieved by upgrading treatment facilities. This includes replacing latrines with actual wastewater treatment plants and making sure that facilities that provide primary treatment — removing solid pollution — also provide secondary treatment — removing organic matter and nutrients with the help of bacteria and microorganisms — and tertiary chemical treatment. Wastewater treatment plants can also be built to capture and reuse biogas.
Direct Removal
While it is important to rapidly move to reduce human-caused methane emissions, some scientists are investigating methods of directly removing methane from the atmosphere to augment these efforts. This can be achieved in two main ways: by bolstering the abilities of natural ecosystems to remove and store methane and through direct geoengineering.
On the ecosystem side, scientists have discovered that tree bark has remarkable methane-absorbing abilities, as it contains organisms called methanotrophs that essentially eat methane. Preserving forests, reforesting or intentionally planting tree species that have greater methane-storing ability could all be ways to take advantage of this nature-based solution.
A potential geoengineering method would be to release iron salt into the atmosphere. This would mimic what happens when dust from Sahara sand storms collides with the sea spray of the Atlantic — instigating a chemical process that breaks down methane. However, more research is required to determine if and how this could be done both safely and effectively. Ultimately, it is safest to rely on the methods that we know work to stop methane from reaching the atmosphere in the first place.
What Progress Has Been Made to Reduce Methane Emissions So Far?
At the COP26 United Nations climate change conference in 2021 in Glasgow, Scotland, the UK and United States launched the Global Methane Pledge. As of January 2025, a total of 159 nations had joined the pledge. Pledge members agreed to work toward cutting global methane emissions by 30% of 2020 levels by 2030. Doing so would be consistent with limiting global warming to 1.5 degrees Celsius above pre-industrial levels and could prevent 0.2 degrees Celsius of warming by 2050. While the pledge’s website claims that it has “generated unprecedented for methane mitigation,” this is yet to manifest in real-world reductions.
Methane emissions broke a new record in 2023, the most recent year for which data is available. Even though the oil and gas sector offers the most possibility for rapid methane cuts, and roughly 80% of that sector falls under a methane-reduction pledge, its total emissions have continued to rise since 2020 and remained past 120 million metric tons per year in 2024. All methane pledges made by governments and companies as of 2023 would in theory be enough to reduce fossil fuel methane emissions by 50% by 2030, but to do this the industry must close its implementation gap. Further, there are major gaps in these commitments. As of 2023, only 13 percent of all methane emissions were covered by any sort of emissions-reduction policy.
What Can Individuals Do to Reduce Methane Emissions?
The two simplest, most effective things that people can do to reduce their individual methane emissions are to switch to lower-methane diets and to reduce their daily food waste through measures such as meal planning, buying “ugly” foods and composting. If you feel intimidated at the thought of going entirely vegetarian or vegan, even just reducing your meat and dairy consumption can make a difference. One study found that if everyone in the European Union limited their meat and dairy consumption by 34%, they would prevent six million metric tons of methane emissions per year.
If you are a homeowner who either cooks on a gas stove or receives heat via a gas furnace, you can replace your gas range with an electric or induction option and swap your furnace for an electric heat pump. Renters may not be able to swap out appliances, but they can still reduce their gas use by finding creative ways to save energy — such as air-drying clothes — or supplementing gas heating and cooking appliances with electric devices like space heaters, rice cookers, microwaves or induction burners.
Ultimately, methane emissions — like all climate pollution — are the products of complex energy, food and waste systems that are kept in place partly because they benefit powerful people who are currently profiting from them. Reducing your personal methane emissions will not remake those systems on its own, but you can also join together with like-minded people to campaign for change. This could range from lobbying your city government to create a municipal composting system to joining or supporting groups like 350.org, Third Act, Oil Change International, Louisiana Bucket Brigade and South Texas Environmental Justice Network that are working to stop the LNG buildout globally, nationally and in their communities.
Takeaway
Methane emissions present both a threat and an opportunity. Because methane is so much more potent than carbon dioxide, it can further turbocharge the global heating that is already raising the thermostat and fueling more extreme storms and other weather events. However, its shorter atmospheric lifespan means that acting urgently to cut its emissions would enable us to make important and timely headway on combating the climate crisis overall. That is why it’s important to spread the word about methane — how it’s released and how to reduce it — and to put pressure on political and business leaders to act on that knowledge.
The post Methane 101: Understanding the Second Most Important Greenhouse Gas appeared first on EcoWatch.
https://www.ecowatch.com/methane-facts-ecowatch.html
Green Living
Mass Die-Off of Western Monarch Butterflies Linked to Pesticides, Study Finds
A new peer-reviewed study has linked pesticides as a likely cause to a mass die-off of Western monarch butterflies that occurred in 2024.
In January 2024, researchers found hundreds of dead or dying monarch butterflies near the Pacific Grove Monarch Sanctuary in California, where Western monarch butterflies typically overwinter.
As The Guardian reported, researchers found the butterflies showing signs of neurotoxic pesticide poisoning, leading to further testing and analysis that has now been published in the journal Environmental Toxicology and Chemistry.
The researchers tested the dead butterflies using liquid and gas chromatography and mass spectrometry, which led the team to find a mix of 15 insecticides, herbicides and fungicides present on the butterflies.
“We found an average of seven different pesticides per butterfly, including multiple insecticides that are highly toxic to insects,” Staci Cibotti, lead author of the study and pesticide risk prevention specialist at Xerces Society for Invertebrate Conservation, said in a statement. “Although a review by Monterey County could not determine the source of the chemicals, the high levels detected suggest that insecticides were likely responsible for the monarch deaths.”
According to the study, three human-made pyrethroid insecticides, including bifenthrin, cypermethrin and permethrin, were found at or near their lethal doses. Further, every sample included bifenthrin and cypermethrin, and all but two samples contained permethrin.
Western monarch butterflies overwinter along the Pacific coast, but they are vulnerable to pesticide residue and drift from nearby farms and urban areas, Cibotti explained.
According to the Xerces Society for Invertebrate Conservation’s annual Western Monarch Count, monarch populations dropped to the second-lowest number ever recorded in 2024, and by 2025, overwintering Western monarchs totaled just 9,119 individuals.
There were already reasons to suspect pesticides for the death of hundreds of monarchs at an overwintering site in 2024, but our new research provides clear evidence of what happened. Each monarch had, on average, 7 different pesticides, many at lethal doses.
xerces.org/press/study-…
— The Xerces Society for Invertebrate Conservation (@xercessociety.bsky.social) July 23, 2025 at 3:31 PM
The Western monarch butterfly population has declined by almost 95% since the 1980s, Xerces Society reported. Migratory monarch butterflies are listed as endangered by the International Union for Conservation of Nature (IUCN), and the U.S. Fish and Wildlife Service estimated that Western monarch butterflies have a 99% chance of becoming extinct by 2080, the Los Angeles Times reported.
As such, preventing the deadly effects of pesticides is a priority for monarch butterfly conservation. Following the study results, Xerces Society has recommended several actions, including increased education about pesticide risks and safer alternatives, establishment of pesticide-free zones around overwintering sites, greater pesticide exposure protections in conservation and recovery plans for butterflies, and stronger coordination and tracking for pesticide risks by public officials.
“Protecting monarchs from pesticides will require both public education and policy change,” Emily May, co-author of the study and agricultural conservation lead at Xerces Society, said in a statement. “We are committed to working with communities and decision-makers to ensure that overwintering sites are healthy refuges for these butterflies.”
The post Mass Die-Off of Western Monarch Butterflies Linked to Pesticides, Study Finds appeared first on EcoWatch.
https://www.ecowatch.com/monarch-butterflies-deaths-pesticides.html
Green Living
Global Hunger Fell Overall in 2024, but Rose in Africa and Western Asia as Climate and Conflict Threaten Progress: UN Report
World hunger fell overall last year, but continued to rise in most of Africa and western Asia, according to a new report — The State of Food Security and Nutrition in the World (SOFI) — published by five specialized UN agencies and released Monday by the Food and Agriculture Organization of the United Nations (FAO).
Roughly 8.2 percent of the world’s population — about 673 million people — suffered from hunger in 2024, a press release from FAO said. The number was down from 8.7 percent in 2022 and 8.5 percent in 2023.
“While it is encouraging to see a decrease in the global hunger rate, we must recognize that progress is uneven. SOFI 2025 serves as a critical reminder that we need to intensify efforts to ensure that everyone has access to sufficient, safe, and nutritious food. To achieve this, we must work collaboratively and innovatively with governments, organizations, and communities to address the specific challenges faced by vulnerable populations, especially in regions where hunger remains persistent,” said FAO Director-General QU Dongyu in the press release.
Between 638 and 720 million people faced hunger in 2024.
Swipe to learn what are the policy solutions to help address the impacts of high food prices on global hunger.
buff.ly/AQA3wsf
#SOFI2025
— Food and Agriculture Organization of the United Nations (@fao.org) July 29, 2025 at 1:31 PM
The report indicates that from 638 to 720 million people faced hunger last year, representing a decrease of approximately 15 million from 2023 and 22 million from 2022.
The number of those who were undernourished in Asia fell to 6.7 percent, down from 7.9 percent two years earlier. The Caribbean and Latin America also saw improvements, with undernourishment decreasing to 5.1 percent of the population — 34 million people — in 2024, following a 2020 peak of 6.1 percent.
“Unfortunately, this positive trend contrasts sharply with the steady rise in hunger across Africa and western Asia, including in many countries affected by prolonged food crises. The proportion of the population facing hunger in Africa surpassed 20 percent in 2024, affecting 307 million people, while in western Asia an estimated 12.7 percent of the population, or more than 39 million people, may have faced hunger in 2024,” FAO said.
At the same time, those experiencing constraints on adequate food access for part of the year — “moderate or severe food insecurity” — decreased to 28 percent in 2024, or 2.3 billion people, down from 28.4 percent in 2023.
“In recent years, the world has made good progress in reducing stunting and supporting exclusive breastfeeding, but there is still much to be done to relieve millions of people from the burdens of food insecurity and malnutrition,” said WHO Director-General Dr. Tedros Adhanom Ghebreyesus.
In low-income countries, 544.7 million people—that’s 72% of the population—couldn’t afford a healthy diet in 2024.
Food is a basic right, not a luxury.
Learn more in the 2025 State of Food Security and Nutrition in the World report
bit.ly/4mjX2nK #SOFI2025
— WHO (@who.int) July 28, 2025 at 12:10 PM
It is estimated that 512 million people could experience chronic undernourishment by 2030, nearly 60 percent of whom will be in Africa. FAO, the International Fund for Agricultural Development (IFAD), the UN World Food Programme (WFP), the United Nations agency for children (UNICEF) and the World Health Organization (WHO) said this highlights the enormous challenge of reaching the Sustainable Development Goal of Zero Hunger.
The report examined the consequences and causes of the food price surge of 2021 to 2023 and its effect on global food security and nutrition. Food price inflation — caused by a combination of the world’s policy response to the COVID-19 pandemic, the impacts of Russia’s war on Ukraine and extreme weather across the globe — has hindered recovery in nutrition and food security since 2020.
Low-income nations have been especially impacted by rising food prices.
“While median global food price inflation increased from 2.3 percent in December 2020 to 13.6 percent in early 2023, it climbed even higher in low-income countries, peaking at 30 percent in May 2023,” FAO said.
But even with rising food prices around the world, the number of those not able to afford to eat a healthy diet fell to 2.6 billion last year, down from 2.76 billion in 2019.
However, in low-income countries, the number of those who couldn’t afford a healthy diet rose to 545 last year, up from 464 million five years earlier. In lower-middle-income nations other than India, the number increased to 869 million from 791 million during the same period.
“In times of rising food prices and disrupted global value chains, we must step up our investments in rural and agricultural transformation. These investments are not only essential for ensuring food and nutrition security – they are also critical for global stability,” said IFAD President Alvaro Lario.
The report recommended a combination of food price inflation policy responses, including transparent and credible monetary policies aimed at containing inflationary pressures; time-bound and targeted fiscal measures like social protection programs to shield vulnerable households; and strategic investing in agrifood research and development, market information systems to boost resilience and productivity and transportation and production infrastructure.
“Every child deserves the chance to grow and thrive. Yet over 190 million children under the age of 5 are affected by undernutrition, which can have negative consequences for their physical and mental development. This robs them of the chance to live to their fullest potential,” said UNICEF Executive Director Catherine Russell. “We must work in collaboration with governments, the private sector and communities themselves to ensure that vulnerable families have access to food that is affordable and with adequate nutrition for children to develop. That includes strengthening social protection programs and teaching parents about locally produced nutritious food for children, including the importance of breastfeeding, which provides the best start to a baby’s life.”
The post Global Hunger Fell Overall in 2024, but Rose in Africa and Western Asia as Climate and Conflict Threaten Progress: UN Report appeared first on EcoWatch.
https://www.ecowatch.com/global-hunger-2024.html
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