Monitoring of extreme land hydrology events in central Poland using GRACE, land surface models and absolute gravity data

被引:6
|
作者
Kuczynska-Siehien, Joanna [1 ,2 ]
Piretzidis, Dimitrios [1 ]
Sideris, Michael G. [1 ]
Olszak, Tomasz [3 ]
Szabo, Viktor [3 ]
机构
[1] Univ Calgary, Dept Geomat Engn, 2500 Univ Dr NW, Calgary, AB T2N 1N4, Canada
[2] Univ Warmia & Mazury, Fac Geodesy Geospatial & Civil Engn, Oczapowskiego 2, Olsztyn, Poland
[3] Warsaw Univ Technol, Fac Geodesy & Cartog, Plac Politech 1, PL-00661 Warsaw, Poland
基金
加拿大自然科学与工程研究理事会;
关键词
Temporal gravity variations; Local hydrology; Flood monitoring; GRACE; GLDAS; Absolute gravimeter; GROUNDWATER DEPLETION; SUPERCONDUCTING GRAVIMETER; CENTRAL-EUROPE; TEMPERATURE VARIABILITY; CLIMATE EXPERIMENT; CORRELATED ERRORS; SPECTRAL-ANALYSIS; DE-CORRELATION; MIDDLE-EAST; SATELLITE;
D O I
10.1515/jag-2019-0003
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
This study deals with the analysis of temporal gravity variations in central Poland, deduced from multiple sources and covering the period from 2002-2016. The gravity data sets used comprise GRACE monthly solutions, GLDAS land surface models and absolute gravimeter measurements from the FG-5 gravimeter located in Jozefos-law, Poland. All data are corrected using standard processing methods in order to include the same gravity effects. After removing the annual and semi-annual components from all data using least-squares spectral analysis and seasonal-trend decomposition, the deseasoned time series are derived and examined for signatures of extreme hydrological events. The signatures of several severe drought and flood conditions affecting Poland and central Europe are identified. A complementary correlation analysis is performed to assess the level of agreement between different data sources. A higher correlation is shown when the analysis is restricted in the 2009-2012 period that includes the 2010 extreme flood and 2011 increased precipitation events, both affecting Poland.
引用
收藏
页码:229 / 243
页数:15
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