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旱区(drylands)是指年平均降雨量与潜在蒸散发之比小于0.65的区域,是最易受气候变化影响的地区之一,生态环境脆弱,荒漠化风险高。中国旱区分布广、类型多。1980-2000年间全球旱区扩张约4%,其中中国旱区扩张面积占比达1/3。针对中国旱区生态系统变化、驱动机制及生态保护与修复工程效应的系统性研究不足,2021年11月9日,北京师范大学地理科学学部傅伯杰院士团队在《自然综述:地球与环境》(...
近日,兰州大学西部环境教育部重点实验室陈发虎院士团队在地学顶级期刊Earth-Science Reviews发表题为“Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climatechange and possible mechanisms on decadal to sub-orbital timescales”...
近日,《中国科学:地球科学》第十一届编委会第一次会议召开,会议遵循科学计量指标定量评价与同行专家定性评审相结合的原则,从每个学科中仅遴选出1篇“热点论文”。兰州大学资源环境学院西部环境教育部重点实验室青年教师黄伟和陈发虎院士等在2015年发表的题为“Definition of the core zone of the “westerlies-dominated climatic regime”, ...
高速远程滑坡(rock avalanches;sturzstorms)作为具有极端破坏力的地质灾害现象,最显著的特征表现在具有巨大的体积(一般在数百万方以上,可达几千万方、几亿方、十几亿方甚至几十亿方、上百亿方)、超常的高速度(迄今为止,已知两个高速远程滑坡的最大速度分别达213 m/s和278 m/s)、难以预料的超常滑距(最大水平滑距Lmax是最大垂直落差Hmax的30倍,甚至更大;滑程可达几...
近日,资源环境学院李育教授及其科研团队在Earth-Science Reviews在线发表了题为“A new assessment of modern climate change, China—An approach based on paleo-climate”的重要研究成果。该研究受到国家自然科学基金项目(41371009,41571178)和兰州大学中央高校基本科研业务费专项资金项目(lz...
在国家自然科学基金重大项目(41590842)和面上项目(41371408)等的资助下,基于城市区位论、城市景观原理和地表辐射能量平衡理论,构建了城市建成区、功能区、不透水地表和绿地覆盖、建筑材质等级地表结构体系,开展了城市不同下垫面地表温度、空气温度、比辐射率、向下短波、反照率、向上/向下长波、潜热、显热和土壤热通量等10个以上参数Landsat TM/MODIS遥感地面同步观测实验,对地表结构...
Please note that all our conferences are non-thematic as explained in our policy (click here). However, academic members and friends can take the lead to organize and chair a panel/session as part of ...
Scott Fendorf Huffington Family Professor in Earth Sciences and Senior Fellow, by courtesy, at the Woods Institute for the Environment,Education Ph.D., University of Delaware, Soil & Environmental...
Associate Professor Kevin Boyce,Stanford School of Earth Energy & Environmental Sciences,Education:Ph.D., Harvard University, Organismic & Evolutionary Biology (2001),B.S., California Institute of Tec...
As with the proverbial canary in the coal mine, birds serve as an indicator of the health of our environment. Many common species have experienced significant population declines within the last 40 ye...
I am a professor in the department of Earth and Atmospheric Sciences, and joined the Cornell faculty in 1980. At that time, I was appointed the Charles L. Pack Research Professor of Forest Soils. My r...
The region between the top of the forest canopy and the base of weathered rock: our living environment and Earth's critical zone.
In our original study we crafted trajectories for developed and developing countries that phased-out greenhouse gas emissions during 2015-2065 such that the maximum global warming does not exceed the ...
A maximum global-mean warming of 2°C above preindustrial temperatures has been adopted by the United Nations Framework Convention on Climate Change to “prevent dangerous anthropogenic interference wit...
The possible response of global climate to the changes of background radiation derived from satellite measurement during 1983-2001 is analyzed. Estimation is made by means of one-dimensional energy-ba...

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