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国家自然科学基金(40605023)

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气候变暖背景下青藏高原植被覆盖特征的时空变化及其成因分析被引量:70
2008年
正交分解反演于NOAA-AVHRR数据的叶面积指数、空间特征场分布和时间系数变化显示,自20世纪80年代初至2000年,在全球变暖气候大背景下,青藏高原地区植被覆盖率总体上呈增加趋势.降水量与主特征场时间系数相关性分析表明,降水量是决定高原地区植被整体覆盖年际变化和波动的主要气候驱动因素.植被覆盖总体增加的同时,高原地区植被覆盖率也存在显著的南北反相位区域变化特征,气候变暖是造成植被覆盖南北反相位变化的主要原因.气温持续增高导致活动积温增加,有利于高原南缘湿润地区植被的生长,相反却使高原北部地区干旱加剧,不利于植被覆盖状况的改善.
徐兴奎陈红LEVY JasonK
关键词:青藏高原叶面积指数正交分解
Spatiotemporal vegetation cover variations in the Qinghai-Tibet Plateau under global climate change被引量:33
2008年
Empirical Orthogonal Function (EOF) analysis and the related Principal Components (PC) analysis are used to extract valuable vegetation cover derived information from the National Oceanic and Atmos- pheric Administration (NOAA-AVHRR)'s Leaf Area Index (LAI) satellite images. Results suggest that from 1982 to 2000 global climate change has contributed to an increase in vegetation cover in the Qinghai-Tibet Plateau. The correlation between rainfall and LAI EOF PC1 and PC2 indicates that rainfall is the major climatic factor influencing interannual variations of average vegetation cover throughout the entire Plateau. However, annual mean vegetation cover trends in the Qinghai-Tibet Plateau are mainly out of phase with air temperature increasing, which is primarily responsible for nonsynchro- nous changes of vegetation cover. In the southern ridge of the Qinghai-Tibet Plateau, recent warming trends contribute to humid weather and favorable conditions for vegetation growth. By contrast, higher temperatures have led to arid conditions and insufficient rainfall in the northern part of the Plateau, leading to drought and other climatic conditions which are not conducive to increased vegetation cover.
XU XingKuiCHEN HongJason K LEVY
关键词:青藏高原植被覆盖率经验正交函数
The Potential Predictability of the South China Sea Summer Monsoon in a Dynamical Seasonal Prediction System被引量:1
2009年
The potential predictability of climatological mean circulation and the interannual variation of the South China Sea summer monsoon (SCSSM) were investigated using hindcast results from the Institute of Atmospheric Physics Dynamical Seasonal Prediction System (IAP DCP),along with the National Centers for Environmental Prediction (NCEP) reanalysis data from the period of 1980-2000.The large-scale characteristics of the SCSSM monthly and seasonal mean low-level circulation have been well reproduced by IAP DCP,especially for the zonal wind at 850 hPa;furthermore,the hindcast variability also agrees quite well with observations.By introducing the South China Sea summer monsoon index,the potential predictability of IAP DCP for the intensity of the SCSSM has been evaluated.IAP DCP showed skill in predicting the interannual variation of SCSSM intensity.The result is highly encouraging;the correlation between the hindcasted and observed SCSSM Index was 0.58,which passes the 95% significance test.The result for the seasonal mean June-July-August SCSSM Index was better than that for the monthly mean,suggesting that seasonal forecasts are more reliable than monthly forecasts.
Chen HongLin Zhao-Hui
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