4.7 Article

A satellite-based approach to estimating spatially distributed groundwater recharge rates in a tropical wet sedimentary region despite cloudy conditions

期刊

JOURNAL OF HYDROLOGY
卷 607, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.jhydrol.2022.127503

关键词

Remote sensing; Water balance; Groundwater recharge; Water table fluctuation; Tropical climate; Sedimentary aquifer

资金

  1. Research Support Foundation of Paraiba State (FAPESQ-PB) [REF: 88887.142311/2017-00]
  2. Newton Fund [2017/2018, REF: 039/2018]
  3. Brazilian Coordination for Improvement of Higher Education Personnel (CAPES) [REF: 88887.161412/2017-00]
  4. Brazilian National Council for Scienti-fic and Technological Development (CNPq) [REF: 433801/2018-2]
  5. Universal MCTI/CNPq [REF: 01.13.0340.00]
  6. Brazilian Innovation Agency (FINEP) [2694, REF: 357874777]
  7. German Research Foundation (DFG)

向作者/读者索取更多资源

Groundwater recharge estimation in tropical wet sedimentary regions is challenging due to limited observed data. This study developed an innovative water budget method using satellite products to estimate spatially distributed groundwater recharge. The results showed that considering cloud-cleaned evapotranspiration and root-zone soil water storage changes are essential for accurate estimation of groundwater recharge in tropical wet sedimentary regions.
Groundwater recharge (GWR) is one of the most challenging water fluxes to estimate, as it relies on observed data that are often limited in many developing countries. This study developed an innovative water budget method using satellite products for estimating the spatially distributed GWR at monthly and annual scales in tropical wet sedimentary regions despite cloudy conditions. The distinctive features proposed in this study include the capacity to address 1) evapotranspiration estimations in tropical wet regions frequently overlaid by substantial cloud cover; and 2) seasonal root-zone water storage estimations in sedimentary regions prone to monthly variations. The method also utilises satellite-based information of the precipitation and surface runoff. The GWR was estimated and validated for the hydrologically contrasting years 2016 and 2017 over a tropical wet sedimentary region located in North-eastern Brazil, which has substantial potential for groundwater abstraction. This study showed that applying a cloud-cleaning procedure based on monthly compositions of biophysical data enables the production of a reasonable proxy for evapotranspiration able to estimate groundwater by the water budget method. The resulting GWR rates were 219 (2016) and 302 (2017) mm yr(-1), showing good correlations (CC = 0.68 to 0.83) and slight underestimations (PBIAS =-13 to-9%) when compared with the referenced estimates obtained by the water table fluctuation method for 23 monitoring wells. Sensitivity analysis shows that water storage changes account for +19% to-22% of our monthly evaluation. The satellite-based approach consistently demonstrated that the consideration of cloud-cleaned evapotranspiration and root-zone soil water storage changes are essential for a proper estimation of spatially distributed GWR in tropical wet sedimentary regions because of their weather seasonality and cloudy conditions.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据