Coupled oceanic-atmospheric variability and U.S. streamflow

Coupled Oceanic-Atmospheric Variability and U.S. Streamflow

Long lead-time streamflow forecasting of the North Platte River incorporating oceanic–atmospheric climate variability

Oceanic-atmospheric variability and western U.S. snowfall

[1] A study of the influences of interdecadal and interannual oceanic-atmospheric influences on April 1 Snow-Water Equivalent (SWE) in the western U.S. is presented. SWE data was identified at 323 Natural Resources Conservation Service (NRCS) SNOTEL (SNOwpack TELemetrysites) stations for the period of 1961 to 2004 and for 121 SNOTEL stations for the period 1941 to 2004. The phases (cold/negativ...

Formation and Variability of a Northerly ITCZ in a Hybrid Coupled AGCM: Continental Forcing and Oceanic–Atmospheric Feedback*

Despite the equatorial symmetry of the annual-mean insolation, the intertropical convergence zone (ITCZ) and the collocated band of high sea surface temperature (SST) assume perennial northern latitudes over the eastern Pacific and Atlantic. An atmospheric general circulation model is coupled with an intermediate ocean model to study continental forcing and oceanic–atmospheric interaction that ...

NOTES AND CORRESPONDENCE Tropical Atmospheric Variability Forced by Oceanic Internal Variability

Atmospheric general circulation model experiments are conducted to quantify the contribution of internal oceanic variability in the form of tropical instability waves (TIWs) to interannual wind and rainfall variability in the tropical Pacific. It is found that in the tropical Pacific, along the equator, and near 25°N and 25°S, TIWs force a significant increase in wind and rainfall variability f...