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The influence of ENSO on global terrestrial water storage using GRACE
Author(s) -
Phillips T.,
Nerem R. S.,
FoxKemper Baylor,
Famiglietti J. S.,
Rajagopalan B.
Publication year - 2012
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2012gl052495
Subject(s) - teleconnection , multivariate enso index , climatology , anomaly (physics) , el niño southern oscillation , la niña , environmental science , structural basin , southern oscillation , lag , geology , geomorphology , computer network , physics , computer science , condensed matter physics
The influence of the El Nino/Southern Oscillation (ENSO) on terrestrial water storage is analyzed for the time period 2003–2010 using monthly estimates of continental water storage from the Gravity Recovery and Climate Experiment (GRACE). Peak correlation between NOAA's Multivariate ENSO Index (MEI) and the measured mass anomaly timeseries shows an R 2 of 0.65 for the Amazon Basin and Borneo in Southeast Asia. By including a Hilbert transformation of the MEI to account for time lag, the R 2 is improved to 0.76. Tropical regions show strong negative correlation with the MEI and arid regions are positively correlated. GRACE is able to detect all the significant known ENSO teleconnection patterns around the globe, including Alaska and Antarctica. In addition, a significant correlation suggests some of Greenland's recent mass loss could be ENSO‐related.