首页|植被状态指数VCI与几种气象干旱指数的对比——以河南省为例

植被状态指数VCI与几种气象干旱指数的对比——以河南省为例

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使用1982-2006年GIMMS AVHRR NDVI数据集与同期的CI、K、Pa、SPI、Z、PDSI等干旱指数做了对比分析,讨论了河南省植被状态指数VCI对气象干旱的滞后效应及干旱监测能力.结果表明:VCI指数与气象干旱指数的相关性受不同下垫面的影响较大,农地的VCI与气象干旱指数相关性要明显高于林地,农地VCI与气象干旱指数呈现正相关关系.在河南省不同的作物生长阶段,VCI对气象干旱有着不同的滞后效应,其中,3-5月份冬小麦生长期VCI对气象条件的反应滞后1~3个月,7、9月份夏玉米生长期VCI对气象条件的反应滞后1月.总体上看,结合前期的气象数据,VCI对河南省气象干旱有一定的指示作用和监测能力.
Comparison of the Vegetation Condition Index with Meteorological Drought Indices: A Case Study in Henan Province
The relationships between satellite-based vegetation condition index (VCI) and a number of frequently used meteorological drought indices,including meteorological drought composite index (CI),K drought index (K),the percentage of precipitation anomalies (Pa),standard precipitation index (SPI),Z-index (Z),Palmer drought severity index (PDSI) were evaluated by using long-term monthly data in Henan Province from 1982 to 2006 in this paper.The temporal lags between VCI and meteorological indices and the capabilities of using VCI to monitor drought is also discussed.The results show that:1) Underlying surface has an impact on the correlations between VCI and meteorological indices.The correlation of VCI with mete orological drought indices of cropland is higher than that of woodland.There is a positive correlation between VCI and meteorological drought indices on cropland.2) There are differences in the temporal lags during different growing stage of crops.During over-winter stage of winter wheat,the lag is one to three months.During summer corn stage,it is one month.The affection of meteorological condition to summer corn is inferior than that to winter wheat.Overall,combining with prophase meteorological condition,VCI is able to indicate meteorological drought and to monitor drought in the province.

vegetation condition index (VCI)drought monitoringland-useHenan Province

沙莎、郭铌、李耀辉、任余龙、李忆平

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中国气象局兰州干旱气象研究所/甘肃省干旱气候变化与减灾重点实验室/中国气象局干旱气候变化与减灾重点实验室,甘肃兰州 730020

VCI 干旱监测 土地利用 河南

公益性行业(气象)科研专项农业部"948"项目

GYHY2010060232011-G9

2013

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCDCSCD北大核心
影响因子:2.546
ISSN:1000-0240
年,卷(期):2013.35(4)
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