Monitoreo de la variación del almacenamiento de agua en la cuenca del Medio y Bajo Paraná a partir de datos GRACE, GRACE FO, TRMM y GLDAS

IF 0.4 Q4 REMOTE SENSING Revista de Teledeteccion Pub Date : 2021-07-21 DOI:10.4995/RAET.2021.15211
Cecilia Cornero, Ayelen Pereira, Ana Cristina Oliveira Cancoro de Matos, María Cristina Pacino, Denizar Blitzkow
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Abstract

GRACE (Gravity Recovery and Climate Experiment) is a satellite mission that can monitor mass distributions in the Earth system, which is closely related to the consequences of climate change. This gravimetric satellite allows to obtain monthly variations of the Earth’s gravity field, which can be associated with water mass variations, after removing the effects of oceanic tides and solid Earth, as well as non-tidal oceanic and atmospheric contributions. In this work, data from GRACE (2002-2017) and GRACE FO (since 2018) were used to analyze the variation of the water mass in the Middle and Low Paraná river basin. The interpretation of the results was carried out by associating the mass anomalies derived from GRACE data with information from the TRMM global rainfall mission. Monthly maps of GRACE water mass variations and TRMM precipitation were produced, which made possible a thorough analysis at a regional level of this mass redistribution in the basin, and its connection to the El Niño and La Niña events that took place in the period under study. The water deficits shown in the 2009 GRACE maps are, in fact, related to the intense episode of La Niña that occurred in the period 2008-2009; while the excess of water storage depicted on the 2016 and 2019 maps is connected to the El Niño phenomenon. Moreover, GRACE has also detected drought events in different sectors between 2011-2012, together with floods in the years 2007 and 2010. Monthly GRACE-derived water storage changes were compared with the independent components of the water balance in the region using different hydrological models estimates. Finally, the temporal variations of the groundwater and the soil part (surface water, soil moisture) were analyzed using the Global Land Data Assimilation System GLDAS. The variables showed a good correlation between them, reaching values of ~r = 0.80.
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利用GRACE、GRACE FO、TRMM和GLDAS数据监测parana中下游流域蓄水变化
GRACE(重力恢复和气候实验)是一项可以监测地球系统质量分布的卫星任务,这与气候变化的后果密切相关。这颗重力卫星可以在消除海洋潮汐和固体地球的影响以及非潮汐海洋和大气的影响后,获得地球重力场的月度变化,这可能与水的质量变化有关。在这项工作中,使用GRACE(2002-2017)和GRACE FO(自2018年以来)的数据来分析中下游巴拉那河流域的水团变化。通过将GRACE数据得出的质量异常与TRMM全球降雨任务的信息联系起来,对结果进行了解释。绘制了GRACE水量变化和TRMM降水量的月度地图,这使得能够在区域层面上彻底分析盆地中的这种质量再分配,以及它与研究期间发生的厄尔尼诺和拉尼娜事件的联系。事实上,2009年GRACE地图中显示的缺水现象与2008-2009年期间发生的强烈拉尼娜现象有关;而2016年和2019年地图上描绘的过量蓄水与厄尔尼诺现象有关。此外,GRACE还发现了2011-2012年间不同部门的干旱事件,以及2007年和2010年的洪水。使用不同的水文模型估计,将GRACE得出的每月蓄水量变化与该地区水平衡的独立组成部分进行比较。最后,利用全球土地数据同化系统GLDAS分析了地下水和土壤部分(地表水、土壤水分)的时间变化。这些变量之间显示出良好的相关性,达到了~r的值 = 0.80。
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来源期刊
Revista de Teledeteccion
Revista de Teledeteccion REMOTE SENSING-
CiteScore
1.80
自引率
14.30%
发文量
11
审稿时长
10 weeks
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