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Drought Monitoring of Southwestern China Using Insufficient GRACE Data for the Long-Term Mean Reference Frame under Global Change

机译:在全球变化下,利用长期平均参考框架使用不足的宽限数据的中国西南部的干旱监测

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Global changes, such as human activities and climate change, increase the odds of worsening drought. The Gravity Recovery and Climate Experiment (GRACE) satellite provides an opportunity to monitor drought levels by the total amount of water, instead of using a small finite set of water cycle elements or indirect indicators. The potential gap lies in the insufficient size of the GRACE record. The database does not meet the requirements of a stationary annual cycle calculated over a relatively long period as recommended by the IPCC, and the disturbance from long-term global changes is often not considered. In this work, a GRACE-based modulated water deficit (GRACE-MWD) process for drought monitoring under the modulated annual cycle (MAC) reference frame in southwest China was proposed. GRACE-MWD achieved a higher ratio of agreement with the standardized precipitation evapotranspiration index at a time scale of 3 months (SPEI03): it ranged from 0.48 to 0.84, while the GRACE-based drought severity index (GRACE-DSI) ranged from 0.48 to 0.68. Compared with remote sensing datasets widely used in drought monitoring, GRACE-MWD data are less affected by seasonality from land-cover categories, which benefit from the MAC reference frame. The ratio-of-agreement metric for the study area showed that GRACE-MWD had a time scale between 7 and 11 months in reference to SPEI and the standardized precipitation index (SPI). The stability of the MAC reference frame to GRACE-MWD was further discussed when GRACE records were extended and was more stable than that of the stationary annual cycle. GRACE-MWD meets global changes via an adaptive reference frame, which is worthy of generalizing to global applications.
机译:人类活动和气候变化等全球变化增加了干旱恶化的可能性。重力恢复和气候实验(GRACE)卫星提供了一个通过总水量监测干旱水平的机会,而不是使用一组有限的水循环元素或间接指标。潜在的差距在于GRACE记录的大小不足。该数据库不符合IPCC建议的在相对较长的时间内计算的固定年周期的要求,并且通常不考虑长期全球变化的干扰。在这项工作中,提出了一种在调制年周期(MAC)坐标系下用于西南地区干旱监测的基于GRACE的调制缺水(GRACE-MWD)过程。GRACE-MWD在3个月的时间尺度上与标准化降水-蒸散指数(SPEI03)的一致性比率更高:它在0.48到0.84之间,而GRACE-DSI在0.48到0.68之间。与干旱监测中广泛使用的遥感数据集相比,GRACE-MWD数据受土地覆盖类别季节性影响较小,这得益于MAC参考框架。研究区域的一致性指标比率表明,相对于SPEI和标准化降水指数(SPI),GRACE-MWD的时间尺度在7到11个月之间。当GRACE记录被扩展时,MAC参考框架对GRACE-MWD的稳定性得到进一步讨论,并且比固定年周期更稳定。GRACE-MWD通过自适应参考框架满足全球变化,值得推广到全球应用。

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