增湿驱动下西北植被物候与水分利用效率变化

IF 3.2 3区 地球科学 Q1 Environmental Science
Wenqing Zhang, Yanling Bai, Liu Liu, Yudong Chen, Jiayi Zhang, Yurui Lun, Xiuping Li
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引用次数: 0

摘要

植被物候是气候变化的重要指标,在生态系统水分利用效率(WUE)中起着平衡固碳和水分流失的重要作用。随着全球气候变化的加速,了解其对物候和水分利用效率的影响对理解生态系统动态和碳-水循环至关重要。中国西北地区是同纬度地区最干旱的地区之一,正经历着由暖干气候向暖湿气候的快速转变,对其脆弱的生态系统构成了重大挑战。利用再分析和卫星遥感资料,分析了1982 - 2015年NWC不同植被类型生长季开始(SOS)、生长季结束(EOS)和生长季长度(LOS)的变化。重点研究了温度和降水变化对物候动态的影响及其对总初级生产力(GPP)、蒸散发(ET)和水分利用效率的后续影响。结果表明:北海道经历了显著的增湿趋势,SOS年平均提前0.04 d, EOS年平均延迟0.04 d,导致LOS年平均延长0.08 d;温度主要驱动SOS的推进,而农田和草原的降水变化以及森林和灌丛的温度变化决定了EOS的延迟。WUE以0.005 gC m−2 mm−1 year−1的速率增加,温度和降水通过物候变化直接或间接影响GPP和ET。这些发现强调了在脆弱的NWC生态系统中,增湿对植被物候和水分利用效率的级联效应。植被生长季节的变化对碳通量和水通量有显著影响,不同植被类型对碳通量和水通量的影响不同。该研究为研究干旱半干旱区植被对快速气候变化的响应机制提供了有价值的见解,并为西北流域水资源和农业的可持续管理提供了重要信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Changes in Vegetation Phenology and Water Use Efficiency Driven by Warming and Wetting in Northwest China

Changes in Vegetation Phenology and Water Use Efficiency Driven by Warming and Wetting in Northwest China

Vegetation phenology is a key indicator of climate change and plays a vital role in ecosystem water use efficiency (WUE), which balances carbon sequestration and water loss. As global climate change accelerates, understanding its effects on phenology and WUE is essential for comprehending ecosystem dynamics and carbon–water cycles. Northwest China (NWC), one of the driest regions at similar latitudes, is experiencing a rapid shift from a warm-dry to a warm-wet climate, posing significant challenges to its fragile ecosystem. In this study, we used reanalysis and satellite remote sensing datasets to analyse the changes in the start of the growing season (SOS), the end of the growing season (EOS) and the length of the growing season (LOS) for various vegetation types in the NWC from 1982 to 2015. The focus was on how temperature and precipitation variations influenced phenological dynamics and their subsequent impacts on Gross Primary Productivity (GPP), evapotranspiration (ET) and WUE. Our results show that NWC has experienced a significant warming and wetting trend, with the SOS advancing by 0.04 days per year and the EOS delaying by 0.04 days per year, leading to a notable extension of the LOS by 0.08 days annually. Temperature primarily drives the SOS advance, while precipitation changes in croplands and grasslands and temperature shifts in forests and shrublands dictate the EOS delays. WUE increased at a rate of 0.005 gC m−2 mm−1 year−1, with temperature and precipitation influencing GPP and ET both directly and indirectly through phenological changes. The findings underscore the cascading effects of warming and wetting on vegetation phenology and WUE in the fragile NWC ecosystem. Changes in the vegetation growing season have had significant impacts on carbon and water fluxes, with varying effects across different vegetation types. This study provides valuable insights into the response mechanisms of vegetation to rapid climate change in arid and semi-arid regions and offers critical information for the sustainable management of water resources and agriculture in the NWC.

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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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