A framework for deriving drought indicators from the Gravity Recovery and Climate Experiment (GRACE)

<p>Identifying and quantifying drought in retrospective is a necessity for better understanding drought conditions and the propagation of drought through the hydrological cycle and eventually for developing forecast systems. Hydrological droughts refer to water deficits in surface and subsurfa...

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Main Authors: H. Gerdener, O. Engels, J. Kusche
Format: Article
Language:English
Published: Copernicus Publications 2020-01-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/24/227/2020/hess-24-227-2020.pdf
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spelling doaj-c57afa2291fb4e4b9d59a70077d506f02020-11-25T01:20:12ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382020-01-012422724810.5194/hess-24-227-2020A framework for deriving drought indicators from the Gravity Recovery and Climate Experiment (GRACE)H. GerdenerO. EngelsJ. Kusche<p>Identifying and quantifying drought in retrospective is a necessity for better understanding drought conditions and the propagation of drought through the hydrological cycle and eventually for developing forecast systems. Hydrological droughts refer to water deficits in surface and subsurface storage, and since these are difficult to monitor at larger scales, several studies have suggested exploiting total water storage data from the GRACE (Gravity Recovery and Climate Experiment) satellite gravity mission to analyze them. This has led to the development of GRACE-based drought indicators. However, it is unclear how the ubiquitous presence of climate-related or anthropogenic water storage trends found within GRACE analyses masks drought signals. Thus, this study aims to better understand how drought signals propagate through GRACE drought indicators in the presence of linear trends, constant accelerations, and GRACE-specific spatial noise. Synthetic data are constructed and existing indicators are modified to possibly improve drought detection. Our results indicate that while the choice of the indicator should be application-dependent, large differences in robustness can be observed. We found a modified, temporally accumulated version of the <span class="cit" id="xref_text.1"><a href="#bib1.bibx64">Zhao et al.</a> (<a href="#bib1.bibx64">2017</a>)</span> indicator particularly robust under realistic simulations. We show that linear trends and constant accelerations seen in GRACE data tend to mask drought signals in indicators and that different spatial averaging methods required to suppress the spatially correlated GRACE noise affect the outcome. Finally, we identify and analyze two droughts in South Africa using real GRACE data and the modified indicators.</p>https://www.hydrol-earth-syst-sci.net/24/227/2020/hess-24-227-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author H. Gerdener
O. Engels
J. Kusche
spellingShingle H. Gerdener
O. Engels
J. Kusche
A framework for deriving drought indicators from the Gravity Recovery and Climate Experiment (GRACE)
Hydrology and Earth System Sciences
author_facet H. Gerdener
O. Engels
J. Kusche
author_sort H. Gerdener
title A framework for deriving drought indicators from the Gravity Recovery and Climate Experiment (GRACE)
title_short A framework for deriving drought indicators from the Gravity Recovery and Climate Experiment (GRACE)
title_full A framework for deriving drought indicators from the Gravity Recovery and Climate Experiment (GRACE)
title_fullStr A framework for deriving drought indicators from the Gravity Recovery and Climate Experiment (GRACE)
title_full_unstemmed A framework for deriving drought indicators from the Gravity Recovery and Climate Experiment (GRACE)
title_sort framework for deriving drought indicators from the gravity recovery and climate experiment (grace)
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2020-01-01
description <p>Identifying and quantifying drought in retrospective is a necessity for better understanding drought conditions and the propagation of drought through the hydrological cycle and eventually for developing forecast systems. Hydrological droughts refer to water deficits in surface and subsurface storage, and since these are difficult to monitor at larger scales, several studies have suggested exploiting total water storage data from the GRACE (Gravity Recovery and Climate Experiment) satellite gravity mission to analyze them. This has led to the development of GRACE-based drought indicators. However, it is unclear how the ubiquitous presence of climate-related or anthropogenic water storage trends found within GRACE analyses masks drought signals. Thus, this study aims to better understand how drought signals propagate through GRACE drought indicators in the presence of linear trends, constant accelerations, and GRACE-specific spatial noise. Synthetic data are constructed and existing indicators are modified to possibly improve drought detection. Our results indicate that while the choice of the indicator should be application-dependent, large differences in robustness can be observed. We found a modified, temporally accumulated version of the <span class="cit" id="xref_text.1"><a href="#bib1.bibx64">Zhao et al.</a> (<a href="#bib1.bibx64">2017</a>)</span> indicator particularly robust under realistic simulations. We show that linear trends and constant accelerations seen in GRACE data tend to mask drought signals in indicators and that different spatial averaging methods required to suppress the spatially correlated GRACE noise affect the outcome. Finally, we identify and analyze two droughts in South Africa using real GRACE data and the modified indicators.</p>
url https://www.hydrol-earth-syst-sci.net/24/227/2020/hess-24-227-2020.pdf
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