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Numerical Evaluation of the Modern and Future Origins of Atmospheric River Moisture Over the West Coast of the United States
Author(s) -
Nusbaumer Jesse,
Noone David
Publication year - 2018
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1029/2017jd028081
Subject(s) - climatology , precipitable water , moisture , environmental science , precipitation , subtropics , subtropical ridge , latitude , atmospheric sciences , oceanography , geography , geology , meteorology , geodesy , fishery , biology
Atmospheric rivers (ARs) are one of the major causes of extreme precipitation and flooding in many regions around the world and have been found to contribute substantially to global poleward moisture transport. However, the evaporative origin of the moisture in ARs remains unclear, at least on climatological timescales. Here we use the water tracer and water isotope‐enabled Community Atmosphere Model version 5 (CAM5) model to examine the moisture sources of ARs that impact the West Coast of the United States. The climatological distribution of moisture sources is determined for both the modern era and for 2100 under a Representative Concentration Pathway (RCP) 8.5 scenario. It is found that 33 to 53% of the precipitable water over the West Coast of the United States originates from the Northeast Pacific, in particular the midlatitudes and subtropics, although in June‐July‐August more moisture is recycled from continental regions. It is also found that although ARs are at least 70% Northeast Pacific moisture, a significant amount of the moisture is derived from tropical latitudes (>15% from south of 20°N). It is found that in the warmer 2100 climate there is a 39% increase in the magnitude of ARs. In this future epoch, moisture is transported from more remote regions for all seasons and for both ARs and the average climatology. To provide future observational evidence that this model result is robust, it is shown that water isotopes provide an observational constraint on the moisture transport pathways, and thus the possibility to observe changes in moisture source.