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On the ability to study regional hydrometeorological changes using GPS and GRACE measurements

Lenczuk, Artur, Olivera-Guerra, Luis, Klos, Anna, and Bogusz, Janusz, 2024. On the ability to study regional hydrometeorological changes using GPS and GRACE measurements. Progress in Earth and Planetary Science, 11(1):63, doi:10.1186/s40645-024-00665-4.

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@ARTICLE{2024PEPS...11...63L,
       author = {{Lenczuk}, Artur and {Olivera-Guerra}, Luis and {Klos}, Anna and {Bogusz}, Janusz},
        title = "{On the ability to study regional hydrometeorological changes using GPS and GRACE measurements}",
      journal = {Progress in Earth and Planetary Science},
     keywords = {GPS, GRACE, Drought, Hydrometeorological events, Climate index, K{\"o}ppen{\textendash}Geiger climate zones},
         year = 2024,
        month = dec,
       volume = {11},
       number = {1},
          eid = {63},
        pages = {63},
     abstract = "{Recently, an ongoing rise in temperature for both land and ocean areas
        is recorded resulting from the Earth's warming climate. As a
        result, droughts we observe are getting more frequent, longer
        and more severe, exerting sustained impacts on humans,
        ecosystems leading to famine, poverty, mass migration, or
        agricultural and economic losses. The changes in climate are
        successfully monitored by analyzing Total Water Storage (TWS).
        For years, TWS has been successfully determined using geodetic
        techniques, such as gravity field variations observed by the
        Gravity Recovery and Climate Experiment (GRACE) missions or
        station position changes monitored by the Global Positioning
        System (GPS). As well, geodetic-derived data can be applied
        successfully to study of hydrometeorological events. To quantify
        droughts characteristics at different temporal and spatial
        scales, we recalculate the vertical displacements to Drought
        Severity Indices (DSI). We find that DSI based on GPS and GRACE
        are positively correlated at over 80\% of stations around the
        world, highlighting both Americas and Europe as the most
        correlated areas. To validate results, we compare DSI based on
        GPS/GRACE with the Global Land Water Storage (GLWS) hydrological
        model, the traditional climate indices, and temperature
        anomalies. We show that GPS-DSIs are strongly temporally
        consistent with both the Standardized Precipitation Index (SPI)
        and the Soil Moisture Index (SMI) climate indices at 85\% of
        stations, indicating weakly correlated areas at mid-latitudes.
        We further show a high potential of geodetic data to assess
        drought characteristics within climate zones as well as global
        studies. We note that moderate conditions dominate for all
        climate zones, for which dry moderate conditions are observed
        for 40\% of the months analyzed. As a result, we note warning
        conditions at least 52\% of global stations with extreme drying
        DSI trends above a value of 2{\textendash}3 per year. We note
        that the global water changes are dominated by 9 month droughts
        at over 72\% of stations, indicating the average drought
        duration around 12, 14, and 15 months for GPS-, GRACE-, and
        GLWS-DSI, respectively. The obtained results from geodetic
        measurements more reliably characterize the type and phase of
        drought, as well as how these droughts cascade into freshwater,
        enabling appropriate mitigation strategies.}",
          doi = {10.1186/s40645-024-00665-4},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2024PEPS...11...63L},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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