首页|青藏高原GPP时空变化特征及影响因素分析

青藏高原GPP时空变化特征及影响因素分析

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研究地表植被GPP时空变化特征及其对气候变化的响应,对深入理解陆地碳循环、评价陆地生态系统的环境质量以及预估未来气候变化的生态效应等具有重大意义.目前青藏高原GPP时空变化研究大多时序较短且未深入分析其时空变化趋势及特征.因此,本研究采用线性趋势探测方法研究青藏高原地区GPP在2001~2019年间的变化特征,并分析该特征对地形和地物类型的响应,同时探索了GPP与气温、降水和积雪的关系.结果表明:青藏高原GPP年际趋势呈现西北低东南高的分布特征,最大值为0.23 gC∙m-2∙d-1,最小值为-0.125 gC∙m-2∙d-1.各月年际趋势中从10月到3月,绝大部分区域GPP年际变化趋势较小,7月GPP的年际变化趋势和空间异质性最大,从-0.384-0.303 gC∙m-2∙d-1,8~10月又逐渐减小.GPP年际趋势随高程的增加逐渐减小;30° N以南GPP年际趋势随纬度的增加迅速减小,30° N以北GPP年际趋势随纬度的增加缓慢增大;农田植被混合类型GPP年际变化增加趋势最大,为 0.034 8 gC∙m-2∙d-1,封闭灌木丛的减小趋势最大,为0.007 6 gC∙m-2∙d-1.近 19 a,气温对青藏高原GPP的贡献最大,其次是降水,辐射再次之,积雪对GPP的贡献相对较弱.
Spatiotemporal Variation Characteristics and Influencing Factors Analysis of the GPP in the Tibetan Plateau
Scientific research on the spatio-temporal variation characteristics of surface vegetation GPP and its response to climate change is of great significance for in-depth understanding of terrestrial carbon cycle,evalua-tion of environmental quality of terrestrial ecosystems,and estimation of the ecological effects of future climate change.At present,most of the time series of GPP spatio-temporal changes on the Qinghai-Tibet Plateau are short and the spatio-temporal changes and characteristics of GPP are not deeply analyzed.Therefore,this study used linear trend detection methods to study the changes of GPP in the Tibetan Plateau between 2001 and 2019,and analyzed the response of this feature to topography and land types,while exploring the relationship between GPP and air temperature,precipitation and snow cover.The results show that the inter-annual trend of GPP on the Tibetan Plateau shows the distribution characteristics of low in northwest and high in southeast,with a maximum value of 0.23 gC∙m-2∙d-1 and a minimum value of-0.125 gC∙m-2∙d-1;From October to March,the inter-annual change trend of GPP in most regions is small.The inter-annual change trend and spatial hetero-geneity of GPP in July is the largest,from-0.384 gC∙m-2∙d-1 to 0.303 gC∙m-2∙d-1,and gradually decrease from August to October.The interannual trend of GPP decreases with elevation increasing.The interannual trend of GPP south of 30° N decreases rapidly and north of 30°N increases slowly with latitude increasing.The increas-ing inter-annual change trend of cropland/natural vegetation mosaics type is largest,0.034 8 gC∙m-2∙d-1.The de-creasing inter-annual change trend of closed shrublands is largest,0.007 6 gC∙m-2∙d-1.In the past 19 years,tem-perature has the largest contribution to the GPP,followed by precipitation,and by radiation again,the contribu-tion of snow to the GPP is relatively weak.

Tibetan PlateauGPPSpatiotemporal changeTopographyLand cover typesClimate factors

李红艳、吴小丹、马杜娟、魏闯、彭博宇、杜炜哲

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兰州大学 资源环境学院,甘肃 兰州 730000

青藏高原 GPP 时空变化 地形 地物类型 气候因子

国家自然科学基金项目国家重点研发计划项目

421611603282019YFA0607003

2024

遥感技术与应用
中国科学院遥感联合中心

遥感技术与应用

CSTPCD北大核心
影响因子:0.961
ISSN:1004-0323
年,卷(期):2024.39(3)
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