• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

了解人类对中国气候变化的影响。

Understanding human influence on climate change in China.

作者信息

Sun Ying, Zhang Xuebin, Ding Yihui, Chen Deliang, Qin Dahe, Zhai Panmao

机构信息

National Climate Center, Laboratory for Climate Studies, Beijing 100081, China.

Climate Research Division, Environment and Climate Change Canada, Toronto M3H 5T4, Canada.

出版信息

Natl Sci Rev. 2021 Jun 29;9(3):nwab113. doi: 10.1093/nsr/nwab113. eCollection 2022 Mar.

DOI:10.1093/nsr/nwab113
PMID:35265337
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8900695/
Abstract

China's climate has been warming since the 1950s, with surface air temperature increasing at a rate higher than the global average. Changes in climate have exerted substantial impacts on water resources, agriculture, ecosystems and human health. Attributing past changes to causes provides a scientific foundation for national and international climate policies. Here, we review recent progress in attributing the observed climate changes over past decades in China. Anthropogenic forcings, dominated by greenhouse gas emissions, are the main drivers for observed increases in mean and extreme temperatures. Evidence of the effect of anthropogenic forcings on precipitation is emerging. Human influence has increased the probability of extreme heat events, and has likely changed the occurrence probabilities for some heavy precipitation events. The way a specific attribution question is posed and the conditions under which the question is addressed present persistent challenges for appropriately communicating attribution results to non-specialists.

摘要

自20世纪50年代以来,中国气候一直在变暖,地表气温上升速度高于全球平均水平。气候变化对水资源、农业、生态系统和人类健康产生了重大影响。将过去的变化归因于各种原因,为国家和国际气候政策提供了科学依据。在此,我们回顾了中国过去几十年观测到的气候变化归因方面的最新进展。以温室气体排放为主的人为强迫是观测到的平均气温和极端气温上升的主要驱动因素。人为强迫对降水影响的证据正在显现。人类影响增加了极端高温事件的发生概率,并且可能改变了一些强降水事件的发生概率。提出特定归因问题的方式以及解决该问题的条件,在向非专业人士恰当地传达归因结果方面一直存在挑战。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/baee414bb12b/nwab113fig7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/b91efd0d92ca/nwab113fig1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/291f9725f47b/nwab113fig2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/e3dd52b84fc5/nwab113fig3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/9493151217c5/nwab113fig4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/128587221d3f/nwab113fig5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/18061eae626f/nwab113fig6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/baee414bb12b/nwab113fig7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/b91efd0d92ca/nwab113fig1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/291f9725f47b/nwab113fig2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/e3dd52b84fc5/nwab113fig3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/9493151217c5/nwab113fig4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/128587221d3f/nwab113fig5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/18061eae626f/nwab113fig6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4538/8900695/baee414bb12b/nwab113fig7.jpg

相似文献

1
Understanding human influence on climate change in China.了解人类对中国气候变化的影响。
Natl Sci Rev. 2021 Jun 29;9(3):nwab113. doi: 10.1093/nsr/nwab113. eCollection 2022 Mar.
2
The 2023 Latin America report of the Countdown on health and climate change: the imperative for health-centred climate-resilient development.《2023年健康与气候变化倒计时拉丁美洲报告:以健康为中心的气候适应型发展的必要性》
Lancet Reg Health Am. 2024 Apr 23;33:100746. doi: 10.1016/j.lana.2024.100746. eCollection 2024 May.
3
Anthropogenic warming has increased drought risk in California.人为变暖增加了加利福尼亚州的干旱风险。
Proc Natl Acad Sci U S A. 2015 Mar 31;112(13):3931-6. doi: 10.1073/pnas.1422385112. Epub 2015 Mar 2.
4
Anthropogenic influence on extremes and risk hotspots.人为影响与极端事件和风险热点
Sci Rep. 2023 Jan 2;13(1):35. doi: 10.1038/s41598-022-27220-9.
5
The impacts of climate change on water resources and agriculture in China.气候变化对中国水资源和农业的影响。
Nature. 2010 Sep 2;467(7311):43-51. doi: 10.1038/nature09364.
6
ARCTIC CHANGE AND POSSIBLE INFLUENCE ON MID-LATITUDE CLIMATE AND WEATHER: A US CLIVAR White Paper.北极变化及其对中纬度气候和天气的可能影响:一份美国气候变率和可预报性研究计划(CLIVAR)白皮书
US CLIVAR Rep. 2018 Mar;n/a. doi: 10.5065/D6TH8KGW.
7
Multifaceted responses of vegetation to average and extreme climate change over global drylands.全球旱地植被对平均和极端气候变化的多方面响应。
Sci Total Environ. 2023 Feb 1;858(Pt 2):159942. doi: 10.1016/j.scitotenv.2022.159942. Epub 2022 Nov 5.
8
Future changes in the intensity and frequency of precipitation extremes over China in a warmer world: Insight from a large ensemble.未来变暖世界中中国极端降水强度和频率的变化:来自大型集合的洞察。
PLoS One. 2021 May 24;16(5):e0252133. doi: 10.1371/journal.pone.0252133. eCollection 2021.
9
Attributing extreme fire risk in Western Canada to human emissions.将加拿大西部的极端火灾风险归因于人类排放。
Clim Change. 2017;144(2):365-379. doi: 10.1007/s10584-017-2030-0. Epub 2017 Jul 15.
10
Changes in climate extremes, fresh water availability and vulnerability to food insecurity projected at 1.5°C and 2°C global warming with a higher-resolution global climate model.采用高分辨率全球气候模型预测在全球升温1.5°C和2°C时极端气候、淡水可利用性及粮食不安全脆弱性的变化。
Philos Trans A Math Phys Eng Sci. 2018 May 13;376(2119). doi: 10.1098/rsta.2016.0452.

引用本文的文献

1
A complex network perspective on spatiotemporal evolution of extreme precipitation over the middle and lower reaches of the Yangtze river.长江中下游极端降水时空演变的复杂网络视角
Sci Rep. 2025 Jul 5;15(1):24056. doi: 10.1038/s41598-025-10146-3.
2
Changes in the annual cycle of surface air temperature over China in the 21st century simulated by CMIP6 models.CMIP6模型模拟的21世纪中国地表气温年循环变化
Sci Rep. 2025 Apr 21;15(1):13661. doi: 10.1038/s41598-025-98672-y.
3
Traditional Meiyu-Baiu has been suspended by global warming.

本文引用的文献

1
Comparison of trends in the Hadley circulation between CMIP6 and CMIP5.CMIP6与CMIP5之间哈得莱环流趋势的比较。
Sci Bull (Beijing). 2020 Oct 15;65(19):1667-1674. doi: 10.1016/j.scib.2020.06.011. Epub 2020 Jun 10.
2
The relationship between latent heating, vertical velocity, and precipitation processes: The impact of aerosols on precipitation in organized deep convective systems.潜热、垂直速度与降水过程之间的关系:气溶胶对有组织深对流系统中降水的影响。
J Geophys Res Atmos. 2016 Jun 16;121(11):6299-6320. doi: 10.1002/2015JD024267. Epub 2016 Apr 6.
3
Human influence has intensified extreme precipitation in North America.
传统的梅雨-白雨现象已因全球变暖而中断。
Natl Sci Rev. 2024 May 15;11(7):nwae166. doi: 10.1093/nsr/nwae166. eCollection 2024 Jul.
4
Impact of temperature on the virulence of in Indonesian aquaculture: A better vaccine design is required.温度对印度尼西亚水产养殖中[病原体名称未给出]毒力的影响:需要更好的疫苗设计。
Vet World. 2024 Mar;17(3):682-689. doi: 10.14202/vetworld.2024.682-689. Epub 2024 Mar 22.
5
Short-term exposure to extreme temperature and outpatient visits for respiratory diseases among children in the northern city of China: a time-series study.中国北方城市儿童短期暴露于极端温度与呼吸疾病门诊就诊的关系:一项时间序列研究。
BMC Public Health. 2024 Feb 1;24(1):341. doi: 10.1186/s12889-024-17814-5.
6
How does Mei-yu precipitation respond to climate change?梅雨降水如何响应气候变化?
Natl Sci Rev. 2023 Sep 18;10(12):nwad246. doi: 10.1093/nsr/nwad246. eCollection 2023 Dec.
7
Impacts of climate change and human activities on vegetation coverage variation in mountainous and hilly areas in Central South of Shandong Province based on tree-ring.基于树木年轮的气候变化和人类活动对鲁中南山区丘陵植被覆盖变化的影响
Front Plant Sci. 2023 Jun 5;14:1158221. doi: 10.3389/fpls.2023.1158221. eCollection 2023.
8
Greenhouse warming and anthropogenic aerosols synergistically reduce springtime rainfall in low-latitude East Asia.温室变暖与人为气溶胶协同减少了东亚低纬度地区的春季降雨量。
NPJ Clim Atmos Sci. 2022;5(1):69. doi: 10.1038/s41612-022-00295-x. Epub 2022 Sep 10.
人类活动加剧了北美的极端降水。
Proc Natl Acad Sci U S A. 2020 Jun 16;117(24):13308-13313. doi: 10.1073/pnas.1921628117. Epub 2020 Jun 1.
4
Anthropogenically-driven increases in the risks of summertime compound hot extremes.人为因素导致夏季复合热浪风险增加。
Nat Commun. 2020 Feb 11;11(1):528. doi: 10.1038/s41467-019-14233-8.
5
Detection and Attribution of Atmospheric Precipitable Water Changes since the 1970s over China.自 20 世纪 70 年代以来中国大气可降水量变化的探测和归因。
Sci Rep. 2019 Nov 26;9(1):17609. doi: 10.1038/s41598-019-54185-z.
6
Storylines: an alternative approach to representing uncertainty in physical aspects of climate change.故事情节:一种在气候变化物理方面表示不确定性的替代方法。
Clim Change. 2018;151(3):555-571. doi: 10.1007/s10584-018-2317-9. Epub 2018 Nov 10.
7
Attribution of extreme weather and climate-related events.极端天气和气候相关事件的归因
Wiley Interdiscip Rev Clim Change. 2016 Jan;7(1):23-41. doi: 10.1002/wcc.380. Epub 2015 Dec 16.
8
Impacts of wind stilling on solar radiation variability in China.静风对中国太阳辐射变化的影响。
Sci Rep. 2015 Oct 14;5:15135. doi: 10.1038/srep15135.
9
Human contribution to more-intense precipitation extremes.人类活动导致降水极端事件更强烈。
Nature. 2011 Feb 17;470(7334):378-81. doi: 10.1038/nature09763.
10
Detection of human influence on twentieth-century precipitation trends.检测人类活动对20世纪降水趋势的影响。
Nature. 2007 Jul 26;448(7152):461-5. doi: 10.1038/nature06025. Epub 2007 Jul 23.