Results 181 to 190 of about 84,446 (258)
Abstract Using a single annual frequency with each year defined from July 1 to June 30 of the following calendar year, this study fits an ellipse to the yearly phase space trajectory of the daily time series of MU (stratospheric mass‐weighted zonally integrated zonal wind at 60°N) and M (total polar stratospheric air mass over 60–90°N) to represent the
Michael Secor +4 more
wiley +1 more source
Volcanic eruptions disrupt ENSO teleconnections with land summer temperature. [PDF]
Zhang X +7 more
europepmc +1 more source
Abstract In Part I, we represent the annual evolution of the Northern Hemisphere stratospheric polar vortex (SPV) in individual years using an ellipse, defined through six ellipse parameters, for the phase‐space trajectory of the daily time series of MU (mass‐weighted zonally integrated zonal wind at 60°N above 400 K) and M (stratospheric air mass over
Michael Secor +4 more
wiley +1 more source
ENSO's changing grip on Bering Sea ice: The emerging control of the North Pacific meridional mode. [PDF]
Chen J +7 more
europepmc +1 more source
Abstract As global circulation models (GCMs) have increased in spatial resolution, more realistic tropical cyclones (TCs) and TC distributions have been simulated. Whereas prior research on TC climatologies has relied on proxies like Potential Intensity and synthetic storm models, the cyclones simulated by newer TC‐resolving GCMs can now be analyzed ...
Andrew Feder +2 more
wiley +1 more source
Increased interannual variability of Sahel rainfall under greenhouse warming. [PDF]
Yang K +6 more
europepmc +1 more source
Enso diversity and global warming
El Niño-Southern Oscillation (ENSO) est le mode de variabilité dominant du Pacifique tropical à l'échelle inter-annuelle. Ce phénomène couplé océan-atmosphère est à l'origine d'événements météorologiques extrêmes qui affectent de nombreuses régions du monde.
openaire +3 more sources
Attribution of Interdecadal Changes in the Spatial Structure of the Spring AO
Abstract The Arctic Oscillation (AO) is one of the key atmospheric circulation modes in the mid‐to‐high latitudes of the Northern Hemisphere. The spatial structure of the spring AO exhibits pronounced interdecadal variation, primarily characterized by a shift of the midlatitude circulation center from the North Pacific Center (NPC) to the North ...
Yanzhu Zheng +3 more
wiley +1 more source
Synergies Between Observed Warming and ENSO Episodes on Extreme Events. [PDF]
Estrada F, Perron P, Yamamoto Y.
europepmc +1 more source

