• 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

气候变化、干扰及由此产生的非线性变化对区域气候变化的影响。

Contributions of changes in climatology and perturbation and the resulting nonlinearity to regional climate change.

机构信息

RIKEN Advanced Institute for Computational Science, 7-1-26 Minatojima-minami-machi, Chuo-ku, Kobe, 650-0047, Japan.

Research Center for Urban Safety and Security, Kobe University, 1-1 Rokkodai, Nada-ku, Kobe, 657-8501, Japan.

出版信息

Nat Commun. 2017 Dec 20;8(1):2224. doi: 10.1038/s41467-017-02360-z.

DOI:10.1038/s41467-017-02360-z
PMID:29263386
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5738341/
Abstract

Future changes in large-scale climatology and perturbation may have different impacts on regional climate change. It is important to understand the impacts of climatology and perturbation in terms of both thermodynamic and dynamic changes. Although many studies have investigated the influence of climatology changes on regional climate, the significance of perturbation changes is still debated. The nonlinear effect of these two changes is also unknown. We propose a systematic procedure that extracts the influences of three factors: changes in climatology, changes in perturbation and the resulting nonlinear effect. We then demonstrate the usefulness of the procedure, applying it to future changes in precipitation. All three factors have the same degree of influence, especially for extreme rainfall events. Thus, regional climate assessments should consider not only the climatology change but also the perturbation change and their nonlinearity. This procedure can advance interpretations of future regional climates.

摘要

未来大规模气候学和摄动变化可能对区域气候变化产生不同的影响。从热力学和动力学变化的角度了解气候学和摄动变化的影响非常重要。尽管许多研究已经调查了气候学变化对区域气候的影响,但摄动变化的意义仍存在争议。这两种变化的非线性效应也未知。我们提出了一种系统的程序,该程序可以提取三个因素的影响:气候学变化、摄动变化以及由此产生的非线性效应。然后,我们通过将其应用于降水的未来变化,展示了该程序的有用性。这三个因素的影响程度相同,特别是对于极端降雨事件。因此,区域气候评估不仅应考虑气候学变化,还应考虑摄动变化及其非线性。该程序可以促进对未来区域气候的解释。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3d77/5738341/58d44fb97a6d/41467_2017_2360_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3d77/5738341/1ab9fa75137a/41467_2017_2360_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3d77/5738341/cfb5c8f2b8d0/41467_2017_2360_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3d77/5738341/fe210acfc4e5/41467_2017_2360_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3d77/5738341/58d44fb97a6d/41467_2017_2360_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3d77/5738341/1ab9fa75137a/41467_2017_2360_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3d77/5738341/cfb5c8f2b8d0/41467_2017_2360_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3d77/5738341/fe210acfc4e5/41467_2017_2360_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3d77/5738341/58d44fb97a6d/41467_2017_2360_Fig4_HTML.jpg

相似文献

1
Contributions of changes in climatology and perturbation and the resulting nonlinearity to regional climate change.气候变化、干扰及由此产生的非线性变化对区域气候变化的影响。
Nat Commun. 2017 Dec 20;8(1):2224. doi: 10.1038/s41467-017-02360-z.
2
Recent and future changes in extreme rainfall in the Catskills region of New York.纽约卡茨基尔地区极端降雨的近期及未来变化
Ann N Y Acad Sci. 2013 Sep;1298:43-51. doi: 10.1111/nyas.12245. Epub 2013 Aug 22.
3
A multi-scale perspective of water pulses in dryland ecosystems: climatology and ecohydrology of the western USA.旱地生态系统中水脉冲的多尺度视角:美国西部的气候学与生态水文学
Oecologia. 2004 Oct;141(2):269-81. doi: 10.1007/s00442-004-1570-y. Epub 2004 May 8.
4
Climatology of salt transitions and implications for stone weathering.盐迁移的气候学及其对石头风化的影响。
Sci Total Environ. 2011 Jun 1;409(13):2577-85. doi: 10.1016/j.scitotenv.2011.03.029. Epub 2011 Apr 22.
5
Capturing subregional variability in regional-scale climate change vulnerability assessments of natural resources.在自然资源区域尺度气候变化脆弱性评估中捕捉次区域变异性。
J Environ Manage. 2016 Mar 15;169:313-8. doi: 10.1016/j.jenvman.2015.12.017. Epub 2016 Jan 19.
6
Assessing future changes in the occurrence of rainfall-induced landslides at a regional scale.评估区域范围内降雨诱发滑坡发生的未来变化。
Sci Total Environ. 2017 Oct 15;596-597:417-426. doi: 10.1016/j.scitotenv.2017.03.103. Epub 2017 Apr 25.
7
The potential impacts of climate variability and change on health impacts of extreme weather events in the United States.气候变率和变化对美国极端天气事件健康影响的潜在影响。
Environ Health Perspect. 2001 May;109 Suppl 2(Suppl 2):191-8. doi: 10.1289/ehp.109-1240666.
8
Multi-century tree-ring precipitation record reveals increasing frequency of extreme dry events in the upper Blue Nile River catchment.多世纪树轮降水记录显示,青尼罗河上游流域极端干旱事件的发生频率正在增加。
Glob Chang Biol. 2017 Dec;23(12):5436-5454. doi: 10.1111/gcb.13809. Epub 2017 Aug 23.
9
Public health consequences of global climate change in the United States--some regions may suffer disproportionately.全球气候变化对美国公共健康的影响——一些地区可能遭受的影响尤为严重。
Environ Health Perspect. 1999 Feb;107 Suppl 1(Suppl 1):169-79. doi: 10.1289/ehp.99107s1169.
10
Regional projections of North Indian climate for adaptation studies.区域预测北印度气候以适应研究。
Sci Total Environ. 2013 Dec 1;468-469 Suppl:S4-17. doi: 10.1016/j.scitotenv.2012.04.066. Epub 2012 May 25.

引用本文的文献

1
Experimental warming and its legacy effects on root dynamics following two hurricane disturbances in a wet tropical forest.实验增温及其在两次热带湿润林飓风干扰后的根系动态滞后效应。
Glob Chang Biol. 2021 Dec;27(24):6423-6435. doi: 10.1111/gcb.15870. Epub 2021 Sep 26.

本文引用的文献

1
The radiative signature of upper tropospheric moistening.对流层上部增湿的辐射特征。
Science. 2005 Nov 4;310(5749):841-4. doi: 10.1126/science.1115602. Epub 2005 Oct 6.
2
More intense, more frequent, and longer lasting heat waves in the 21st century.21世纪热浪更加剧烈、更加频繁且持续时间更长。
Science. 2004 Aug 13;305(5686):994-7. doi: 10.1126/science.1098704.
3
Constraints on future changes in climate and the hydrologic cycle.对未来气候和水文循环变化的限制。
Nature. 2002 Sep 12;419(6903):224-32. doi: 10.1038/nature01092.