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暴雨、洪水和热浪等极端天气事件被称为中国的“新常态”。

今年四月的暴雨和洪水导致中国损失近120亿元人民币(16.5亿美元),灾害损失“为近10年同期最重”。六月,中国约有33条河流“超过警戒水位”,数十人丧生。广西桂林遭遇自1998年以来最大洪水。

不到一年前,北京气象部门在2023年7月的短短五天内记录了745毫米的降雨量,几乎是该市往年整月的降雨量。

北京周边的河北省在同一时间也出现了强降雨。2023年7月,临城县的降雨量超过1米,是其年平均降雨量的两倍。

2021年7月,河北的邻省河南出现了“千年一遇”的暴雨。

虽然中国已经出台了更多政策来改善其应急系统和基础设施,但日益增多的极端天气事件仍继续带来挑战。

在本篇Q&A中,Carbon Brief将探讨中国近期洪灾的原因、中国如何适应洪灾,以及是否需要未雨绸缪、重新审视其防洪系统。

近期洪灾背后的原因是什么?

近年来频繁发生的暴雨和洪水背后有各种因素。

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英国布里斯托尔大学地理科学学院名誉研究员奥利弗·温(Oliver Wing)博士告诉Carbon Brief:“总体而言,由于克劳修斯-克拉佩龙方程,我们预计气候变暖的世界将更加湿润。”

根据该方程,气温每升高1°C,空气中的湿度通常会增加约7%,这意味着气候变暖时降雨量可能会更大。

奥利弗·温指出,“对于日以下降雨量,我们看到的比例关系比该方程所显示的还要大。这使得地表水(更有可能)由于短时和高强度的局部降雨增加而在城市形成洪水”。

此外,他表示,“气候变暖正导致大多数地方的海平面上升,这意味着风暴潮造成破坏的基线更高”。

据《中国日报》引述中国气象局国家气候中心首席预报员郑志海称,自四月份以来,中国广东和广西等南部沿海省份频繁出现强降雨,其原因是“高于正常水平的温度”。

郑志海补充说,厄尔尼诺/南方涛动(在2023年中期进入厄尔尼诺升温阶段的自然气候周期)是部分原因,因为其提高了海面温度,并将大量水蒸气从南中国海和孟加拉湾引向中国南部。

宁波诺丁汉大学地理科学系系主任陈加信博士告诉Carbon Brief,今年4月广东的降雨模式与2023年9月6日至8日台风“海葵”过后的强降雨十分相似。

具体而言,强降雨是由来自东南亚和南亚季风模态中的低压湿气流,与来自菲律宾和西太平洋的另一个低压雨带碰撞产生的。

台风“海葵”给香港带来了140年来最严重的暴风雨,并在广东和福建两省造成了最严重的降雨。

陈加信表示,虽然在气象学意义上这些强烈暴风雨并不罕见,但由于全球变暖,其发生的频率越来越高。

四月是季风季的开始。大范围的暴风雨通常在四月平均发生三次。但是,今年中国仅在该月就遭受了至少八次区域性极端降雨事件侵袭,而且都是接连发生的。

在重庆和湖南等受影响地区,河流洪水的现象十分普遍。对于一般的河流洪水来说,确定原因可能更为复杂。

“有很多调节因素。在气候变暖的情况下,较干燥的土壤可能会使土地吸收更多降雨,从而减轻洪水带来的危害。许多洪水不是由强降雨造成,而是由融雪或落在饱和土壤上的低强度、长时间降雨造成的。 因此,单凭气候变暖导致降雨量增加不能合理推断出河流洪水也会增加。”奥利弗·温说。

陈加信表示,自然原因“当然”增加了湿度,“但人类引起的气候变化导致温室效应,造成海水温度上升,从而引起更多的风暴和低压雨带。这是事实。”

奥利弗·温同意,人类导致的气候变化的“热力学影响”增加了与风暴相关的降雨量。

但他补充道:“我们不甚了解的是,人为气候变化如何改变了气候系统的动态,以及这种变化在哪里和如何加剧或抑制了热力学响应。”

人类导致的气候变化起了什么作用?

许多研究发现,海面温度升高正在加剧高强度的连续极端降雨。

联合国政府间气候变化专门委员会(IPCC)的第六次评估报告(AR6)也指出,温室气体排放造成的人为气候变化导致海洋变暖,这也“很可能是已观测到的全球陆地强降水加剧的主要驱动因素”。

根据第六次评估报告,在全球相比工业化前升温1.5°C的情况下,东亚和中亚极端年最大日降雨量(Rx1)和五日累积降雨量(Rx5)预计将比1971年至2000年分别增加28%和15%。

该报告还指出,与之类似的是,在中国的城市群中,“全球从升温1.5°C增加到2°C可能会使非常潮湿日子的总降水强度增加1.8倍,最大五日降水量增加一倍”。

中国气象局中国气象科学研究院的陈阳教授告诉Carbon Brief,中国人为造成的强降雨的强度甚至超过预期。

“由于气候变暖导致大气湿度增加,潜热释放与潮湿风暴中的上升运动之间的反馈作用更强,因此人为造成的中国季风区强降水的加剧程度明显大于预期。”他解释说。

他补充说,与纬度相似的其他地区相比,这种反馈在中国东部尤为明显。

最近发表在《自然》上的一项研究还预计,由于气候变暖,中国的风暴活动将变得更加频繁和剧烈。研究显示,到21世纪末,中国东部沿海热带气旋的年平均发生频率预计将比现在增加16%。

A woman wearing a traditional costume during a hot day in Beijing, China.
在中国北京炙热的天气里,一名女子身着汉服。图片来源:Associated Press / Alamy Stock Photo

除了人类活动引发的气候变化之外,城市设计和建造不当,以及地下水开采、城市发展导致的建筑物重量、城市交通系统和采矿活动造成的沉降,也会加剧洪灾。

美国路易斯安那州立大学社会学系助理教授凯文·斯迈利(Kevin Smiley)博士告诉Carbon Brief:“气候变化正在加剧极端天气的严重程度和频率。由气候变化引起的额外降雨可能会导致原本只是建筑物的停车场在下雨天出现水坑,而现在洪水会漫过建筑物大门,造成数千美元的损失。”

“重要的是要记住:气候变化是人为的,所以这种风险的增加也有人为的根源。”

中国如何适应日益频繁的洪水?

中国修建了许多大型水利工程来防止洪涝灾害,例如2002年启动的从长江取水的南水北调工程。

在中国国务院最新公布的《国家水网建设规划纲要》中,在2035年前建成“国家水网”是未来防洪的“骨干”措施之一。

文件中的“骨干”工程还包括主要河流上的大型硬工程结构,如堤防、防洪闸和河道泄洪网络,以减轻洪水风险。

与此同时,发表在《海洋与海岸管理》(Ocean & Coastal Management)杂志上的一项研究发现,“基于自然的解决方案”在中国也变得流行起来。

沿海岸线和河口恢复和保护淡水沼泽、红树林和湿地,正在被用来为潮汐和风暴潮提供缓冲。它们包括上海的崇明岛湿地(长江三角洲)和深圳湾的福田和米埔湿地(珠江三角洲)。

规划文件中提出的另一个概念是“加快智慧发展”,利用互联网、数据和技术来监测和预防洪水。

首都北京已整合高清摄像机、望远镜、雷达图和卫星云图的数据,以提供实时灾害更新,从而改善应急响应时间。

中国东部港口城市宁波与电信公司合作,分析大数据并发布信息。

应急管理部表示,这些措施使2018年至2022年因自然灾害造成的死亡和失踪人数与2013年至2017年相比减少了54%。2023年,死亡人数继续下降,但与2018年至2022年水平相比,被毁建筑物数量和直接经济损失分别上升了97%和13%。

2015年,海绵城市的概念被写入住房和城乡建设部的政策文件。该计划在全国推广,武汉(1100万人口)、郑州(1000万人口)等30个主要城市被选为试点城市。

Aerial photo of Huangtaihu Lake, Qian'an City, China.
中国迁安市黄台湖。图片来源:Xinhua / Alamy Stock Photo

这些海绵城市旨在通过城市地区的“绿蓝设施”,如绿色屋顶、透水路面和雨水公园,收集、净化和再利用至少70%的洪水。整个系统旨在一次性解决城市供暖、淡水匮乏和洪水泛滥等问题。

中国也改进了其恢复过程。例如,在2021年台风“烟花”期间,宁波的洪灾受害者通过改进的在线文件系统,在一小时内就能获得经济补偿。

这些措施效果如何?

陈加信告诉 Carbon Brief,中国“在洪水和干旱灾害的准备、应对和恢复方面做得非常好”,这是两种最具破坏性的自然灾害。

“作为一个全球南方国家,”他将中国称为发展中国家,“中国用海绵城市和增强生态的解决方案应对气候变化,做得相当不错”。

然而,温认为,基于自然的解决方案,如海绵城市,可能会“很快饱和”,因此“它们的作用可能会被夸大”。他继续说:

“这些类型的干预措施对于相对频繁的低强度降雨最有效。在非常强烈、罕见的降雨(其概率在全球变暖的情况下迅速变化)期间,它们将很快不堪重负,造成最大的破坏和痛苦。”

2021 年,一场“历史罕见”的暴雨和洪水影响了海绵城市郑州 1400 多万人,造成 398 人死亡,凸显了海绵城市在气候变化面前的局限性。

《自然》杂志的研究称,海绵城市的设计只能承受 30 年一遇的降雨事件。陈加信说,除此之外,它还会造成一种虚假的安全感。它鼓励更多人迁往高风险地区,导致这些地区的人口和资产增加,而这些聚集地的保护需求也应声而涨,形成一种被称为“堤坝效应”的循环。

堤坝效应是一种悖论:修建防洪堤坝会导致人们对洪水风险的认知降低,业主更有可能投资于自己的房产,从而增加堤坝决口时的潜在损失。

根据《自然》杂志的论文,洪水的影响是人口稠密的黄河三角洲和珠江流域面临的一个关键挑战,这两个地区都面临着很高的洪水风险。

斯迈利说:“当社会的脆弱性与灾害交织在一起时,风险就会显现出来。脆弱性是社会性的,社会脆弱性越大,洪水的影响就越大……社会的脆弱性还是不公平的。一个有一定财富和良好保险的家庭,比一个靠薪水度日的家庭能更快、更成功地从洪水中恢复过来。”

中国政府通过特别政府债券拨款超过一万亿元人民币(1380 亿美元),用于支持弱势公民和今年 3 月遭受自然灾害的地区重建。据官方媒体《环球时报》报道,超过一半的资金将用于“防洪等水利工程建设”。

但过去,财政支持的提供一直受到质疑。全球再保险公司慕尼黑再保险(Munich Re)称,2023 年台风杜苏芮袭击中国时,在总计约 250 亿美元的损失中,只有 20 亿美元得到了承保。

此外,2015 年至 2018 年间,这些海绵城市的建设已经花费了中国 15-18 亿元人民币(2.1-2.5 亿美元)。维护费用将使这笔费用更高。

《自然》杂志的作者建议政府应致力于将分散的“灰色基础设施”(排水沟、管道和泵站等建筑结构)整合到现有的绿色蓝色设施中,但不应仅仅依赖工程基础设施。

中国科学院西北生态环境资源研究所研究员舒乐乐博士告诉《知识分子》杂志:“仅靠传统的工程方法无法减轻目前强降雨的影响”。

“每次下大雨,它造成的损失都会成为头条新闻,主要是因为城市里住着太多人,”舒补充道。

洪水易发地区的政府部门合作不当也导致灾害管理缺乏统一调配。

《自然》杂志的研究补充说,就长江和珠江三角洲而言,其缺乏一个覆盖全区的、且可以“把地划分土和投资融合起来的水文系统”。

中国社会科学院生态文明研究所研究员郑艳博士在 2023 年北京洪水过后指出,政府机构往往只顾自己的管辖范围,只想着转移问题,迅速疏导洪水,这给下游地区的城市带来了压力。

斯迈利说:“洪水不会在意人为划定的市、区或省的边界。一个地方有效的城市设计可能会减轻那里的洪水风险,但会间接增加其他地方的风险。以正义为中心、集体思考(统一筹划)可以提供一个本地化的解决方案来帮助所有人有效恢复,而不是加剧不平等。”

中国可以从其他城市学到什么?

洪水是世界各地城市都面临的挑战,中国因此可以借鉴大量的想法和技术。

《自然》杂志的论文建议,长江三角洲和珠江三角洲可以向恒河-布拉马普特拉河-梅格纳河三角洲和湄公河三角洲学习,“通过利用和调整因气候变化和人类活动而迅速变化的三角洲潜在动态,改善其对沉降和侵蚀等区域挑战的应对”。

该论文还提倡建设一个“积极主动、具有前瞻性、具有足够能力限制洪水破坏性影响并及时恢复灾前状态”的弹性社会。

鹿特丹是一座四面环水、人口 60 万的荷兰三角洲城市。鹿特丹建造了蓄水设施,例如具有蓄水功能、面积相当于四个奥林匹克游泳池的地下停车场, 且安装了绿色屋顶和外墙来吸收雨水。

日本在东京郊区埼玉县在地下建造了一个复杂的混凝土隧道和拱顶网络。这个网络位于大约地下 14 层,可容纳的雨水可以装满 1,000 多个奥运会标准泳池。

这两个城市的地下洪水转移设施经常被用作气候变化前沿城市可行的防洪系统的典范。

香港在跑马地马场的下方也有一个类似的地下雨水储存系统,旨在抵御 50 年一遇的洪水事件。

然而,陈加信表示,防洪措施的有效性难以横向比较,因为每个城市的地理、人口、密度和地形都非常不同。

他告诉 Carbon Brief:“在我看来,中国的特大城市应该考虑利用地下空间来储存超强暴雨突然排放的极端雨水……东京和鹿特丹利用地下空间的做法就相当明智。”

The post Q&A:中国如何适应日益频繁的洪灾 appeared first on Carbon Brief.

https://www.carbonbrief.org/qa%ef%bc%9a%e4%b8%ad%e5%9b%bd%e5%a6%82%e4%bd%95%e9%80%82%e5%ba%94%e6%97%a5%e7%9b%8a%e9%a2%91%e7%b9%81%e7%9a%84%e6%b4%aa%e7%81%be/

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Climate Change

Every country needs a model to help optimise its energy transition

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Claver Gatete is Executive Secretary of the UN Economic Commission for Africa. Jason Veysey is Energy Modeling Program Director and Senior Scientist at the Stockholm Environment Institute. Lisa Sachs is Director of the Columbia Center on Sustainable Investment at Columbia University.

The case for global energy transition has rarely been clearer. The closure of the Strait of Hormuz earlier this year exposed the cost of unplanned, fossil-dependent systems, while the falling cost of renewables, the rising penetration of electric vehicles, and the growing value of demand flexibility have made the direction of travel obvious. The benefits of a clean, secure, integrated system are no longer in dispute. What remains unclear is how to build it.

Countries around the world have called for faster renewable energy deployment and alternative energy arrangements. A secure, affordable, resilient, decarbonised system requires specific investments in specific places in a specific sequence, optimised across sectors and borders. But very few governments have the analytical foundation to translate those imperatives into investment.

The two instruments that are supposed to determine investment priorities for decarbonisation – Nationally Determined Contributions (NDCs) and country platforms – cannot answer the most basic question facing any country undertaking an energy transition: what should the energy system look like?

    To close this gap, every country needs a bankable, economy-wide optimisation model for its energy system. A model is not a plan, but it can help answer the critical question of what the future energy system should look like. It shows how optimal scenarios vary as assumptions and policies are adjusted, calculates investment requirements and sequencing, and quantifies how system costs are affected by assumptions, policies, and exogenous variables like trade policy and financing terms.

    Tool for efficient investment

    Optimisation is a simplified way of simulating an energy system, but it can be an extremely powerful tool for moving energy planning from reactive (how do we manage the disparate actions in the energy system?) to intentional (what energy system underpins our national objectives?). A model can show how optimal scenarios vary as assumptions and policies are adjusted, and how investment requirements are quantified and sequenced.

    Optimisation models can treat the energy system and the sectors it serves as an integrated whole, optimising across sectors and projects in ways that can be mutually reinforcing. If considered independently, growth in industrial demand, transport electrification, and digital infrastructure can add stress to the energy system. But an optimised plan can arrange these and other changes in an efficient, synergistic way.

    Two to tango: How governments can unlock private investment for national climate goals

    New load can be added where low-cost power is available; industrial customers can ensure the viability of investments in energy supply; electric vehicle charging policy can smooth load curves and reduce costs for all consumers.

    Additionally, optimisation modeling can also change the financeability of investments. Taken alone, each project faces uncertainty about the rest of the system, which raises the cost of capital and causes projects to stall or unwind after contracts are signed. A coherent, optimised plan makes visible the coordination that private capital would otherwise have to bet on: identified offtake, sequenced and committed transmission, contracted power supply, and so on.

    What COP31 and COP32 should do

    The upcoming COPs in Turkey and Ethiopia can shift the center of gravity of international climate cooperation from fragmented commitments to planning. Three moves are urgently needed.

    First, optimised, economy-wide, long-term energy system planning must be the foundation on which any meaningful NDC, country platform, or finance commitment rests. NDCs are typically drafted by environment or single-line ministries, with limited cross-sectoral input from ministries of energy, finance, and planning. They contain targets, derived from sectoral strategies or national commitments, not from an analytically grounded picture of what the energy system should look like and what investments would make it work. Country platforms are generally a portfolio of investments assembled from existing project pipelines, rather than derived from a system-level analysis of what an optimised, decarbonised energy system would require.

    Second, recognise regions as a key planning unit. Modern integrated energy systems are inherently regional. Renewable endowments are unevenly distributed; balancing variable supply across borders lowers aggregate cost, reduces redundant backup capacity, and unlocks economies of scale no individual nation can achieve. Many energy investments in Southeast Asia, East Africa, Southern Africa and Central Asia may only be financeable in a regional context. Assessing domestic infrastructure without regional optimisation perpetuates the perception that decarbonisation is more expensive than it is.

    COP31 leaders unveil global targets, with spotlight on electrification

    Third, finance the planning capacity. A coordinated commitment by multilateral development banks, bilateral donors, and philanthropic partners to help every region and its constituent countries develop and maintain their own modelling capability, with open-source tools and regional analytical hubs, would close the most consequential gap in the current architecture. The cost is small relative to current spending on country platforms, failed project preparation, and misallocated infrastructure investment.

    This includes supporting regional institutions such as the ASEAN Centre for Energy, the African Energy Commission, regional power pools, and the Latin American and Caribbean Energy Organization to determine what optimised regional systems require. Country-by-country pledging, repeated at every COP, will not deliver what meaningfully integrated systems can.

    The 2026 energy crisis made the cost of unplanned, fossil-dependent systems newly visible. That window of clarity will close. The international community should seize the moment to build the planning foundation that has been missing for thirty years, rather than commissioning another round of NDCs or pledges, striving for outcomes neither was designed to deliver.

    The post Every country needs a model to help optimise its energy transition appeared first on Climate Home News.

    Every country needs a model to help optimise its energy transition

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    Explainer: How the ‘super El Niño’ will reshape the world’s weather

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    The world is currently experiencing what is expected to become the strongest El Niño on record – dubbed a “super El Niño” by many.

    El Niño is the warm phase of a recurring climate pattern in the tropical Pacific that releases heat from the ocean into the atmosphere.

    This temporarily raises global temperatures and reshapes rainfall and extreme weather around the world – impacting the lives of billions of people.

    The current El Niño event began in June and is expected to last into 2027.

    El Niño is part of a wider climate pattern called the El Niño-Southern Oscillation (ENSO) cycle.

    The ENSO cycle also has a cool phase, known as La Niña, as well as a “neutral” phase. El Niño and La Niña events typically last between nine and 12 months, but can go on longer.

    Below, Carbon Brief explains how the ENSO cycle works, its impacts on extreme weather and global temperatures and why this El Niño event is projected to be the most intense since records began.

    The post Explainer: How the ‘super El Niño’ will reshape the world’s weather appeared first on Carbon Brief.

    https://interactive.carbonbrief.org/el-nino-explainer/index.html

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    Analysis: The two largest reservoirs in the US have hit record-low levels

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    The second-largest reservoir in the US reached a record-low water height on Saturday – just days after the country’s largest reservoir broke its own record. 

    Both Lake Mead and Lake Powell are located on the Colorado River.

    They provide water for populations across seven US states in the south-western US, with around 40 million people getting some or all of their municipal water from the Colorado River.

    The river also provides water for around 5.5m acres (22,258 square kilometres) of farmland across Colorado, Arizona, California and the other states in the river basin.

    Experts tell Carbon Brief that climate change, population growth and over-consumption are all contributing to the current record-low levels of the reservoirs.

    Record lows

    At full capacity, Lakes Mead and Powell can hold a combined 68 cubic kilometres of water – enough to supply all household consumption in the contiguous US for nearly 1.5 years. However, the water level in both reservoirs has been declining for decades.

    The chart below shows the water level of Lake Mead, in metres above mean sea level. The reservoir, which began to fill in 1935 following the construction of the Hoover Dam, has a “full pool” maximum capacity of 347.60 metres. The water level in Lake Mead reached a record low of 317.11 metres on 7 August.

    Lake Mead, the larges reservoir in the US, reached record-low water levels in early August.

    The following chart shows the water level of Lake Powell, in metres above mean sea level. Lake Powell’s full-pool level is 1,127.76 metres.

    While the reservoir reached its maximum capacity several times in the 1980s, it has not done so since. On 15 August, the water level in Lake Powell was recorded at a new record-low of 1,072.87 metres.

    Lake Powell, the second-largest reservoir in the US, reached record-low water levels in mid-August

    Both reservoirs have continued to decline in the days since breaking their respective records. The downward trend will largely continue in both lakes until next spring, when the snowpack in the mountains of the Upper Colorado River Basin begins to melt, says Dr Jack Schmidt, a senior research scientist at Utah State University’s Center for Colorado River Studies. He tells Carbon Brief:

    “The big dilemma of the moment is that we’re only in the middle of August, and we have no assurance of what the coming winter will be. The only thing we can be sure of is that we will be depleting overall total basin reservoir storage from now until, roughly, early April.”

    Compounding factors

    The record lows across the two reservoirs are the result of several compounding factors, experts tell Carbon Brief.

    Since the turn of the 20th century, the amount of water flowing along the Upper Colorado River has declined by about 20%. Research suggests that half of this decline can be attributed to human-induced climate change.

    Most of the river’s streamflow comes from the snowpack of the Upper Colorado River Basin, which stretches across five western US states but is primarily located in Colorado and Utah.

    This region has been gripped by a historic “megadrought” for more than a quarter of a century. Nearly half of the megadrought’s intensity over 2000-18 is attributable to climate change, according to a 2020 study.

    At the same time, the increasing population in the US south-west has put added pressure on the Colorado River’s water supply. The number of people obtaining some or all of their water from the Colorado system has grown by 15 million (around 60%) since 1992.

    Schmidt tells Carbon Brief:

    “There’s an ultimate cause of the present water crisis, and there’s a proximate cause. The ultimate cause is a warming climate, a warming planet and a pretty clear correlation between warming conditions and decreased runoff in the Colorado River Basin.

    “The proximate cause is that in this messy democratic republic of ours, big policy decisions that match the variability of the climate occur painfully slowly – with intense political negotiations – and only incrementally.”

    On 31 July, the US Bureau of Reclamation, which manages water resources in the western US, released an environmental impact statement on its proposed post-2026 strategy for managing Lakes Powell and Mead. The strategy itself has not been released yet.

    Schmidt notes that the statement does appear to give the Bureau flexibility to “respond to crisis” by reducing the delivery of water to several states. However, he adds:

    “They acknowledge it won’t work if we just stay critically dry, and of course every climate model for the 21st century, especially with a continually warming planet, says that that’s exactly what’s going to happen.”

    The post Analysis: The two largest reservoirs in the US have hit record-low levels appeared first on Carbon Brief.

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