Thu Dec 12, F.Flechtner
• Sorted by Date • Sorted by Last Name of First Author •
Rodell, Matthew, Barnoud, Anne, Robertson, Franklin R., Allan, Richard P., Bellas-Manley, Ashley, Bosilovich, Michael G., Chambers, Don, Landerer, Felix, Loomis, Bryant, Nerem, R. Steven, O'Neill, Mary Michael, Wiese, David, and Seneviratne, Sonia I., 2024. An Abrupt Decline in Global Terrestrial Water Storage and Its Relationship with Sea Level Change. Surveys in Geophysics, .
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2024SGeo..tmp...74R,
author = {{Rodell}, Matthew and {Barnoud}, Anne and {Robertson}, Franklin R. and {Allan}, Richard P. and {Bellas-Manley}, Ashley and {Bosilovich}, Michael G. and {Chambers}, Don and {Landerer}, Felix and {Loomis}, Bryant and {Nerem}, R. Steven and {O'Neill}, Mary Michael and {Wiese}, David and {Seneviratne}, Sonia I.},
title = "{An Abrupt Decline in Global Terrestrial Water Storage and Its Relationship with Sea Level Change}",
journal = {Surveys in Geophysics},
keywords = {Climate change, Terrestrial water storage, Sea level, GRACE},
year = 2024,
month = nov,
abstract = "{As observed by the Gravity Recovery and Climate Experiment (GRACE) and
GRACE Follow On (GRACE-FO) missions, global terrestrial water
storage (TWS), excluding ice sheets and glaciers, declined
rapidly between May 2014 and March 2016. By 2023, it had not yet
recovered, with the upper end of its range remaining 1 cm
equivalent height of water below the upper end of the earlier
range. Beginning with a record-setting drought in northeastern
South America, a series of droughts on five continents helped to
prevent global TWS from rebounding. While back-to-back El
Ni{\~n}o events are largely responsible for the South American
drought and others in the 2014-2016 timeframe, the possibility
exists that global warming has contributed to a net drying of
the land since then, through enhanced evapotranspiration and
increasing frequency and intensity of drought. Corollary to the
decline in global TWS since 2015 has been a rise in barystatic
sea level (i.e., global mean ocean mass). However, we find no
evidence that it is anything other than a coincidence that, also
in 2015, two estimates of barystatic sea level change, one from
GRACE/FO and the other from a combination of satellite altimetry
and Argo float ocean temperature measurements, began to diverge.
Herein, we discuss both the mechanisms that account for the
abrupt decline in terrestrial water storage and the possible
explanations for the divergence of the barystatic sea level
change estimates.}",
doi = {10.1007/s10712-024-09860-w},
adsurl = {https://ui.adsabs.harvard.edu/abs/2024SGeo..tmp...74R},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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