The teleconnection of El Niño Southern Oscillation to the stratosphere
DIV Domeisen, CI Garfinkel… - Reviews of Geophysics, 2019 - Wiley Online Library
El Niño and La Niña events in the tropical Pacific have significant and disrupting impacts on
the global atmospheric and oceanic circulation. El Niño Southern Oscillation (ENSO) …
the global atmospheric and oceanic circulation. El Niño Southern Oscillation (ENSO) …
ENSO atmospheric teleconnections and their response to greenhouse gas forcing
El Niño and Southern Oscillation (ENSO) is the most prominent year‐to‐year climate
fluctuation on Earth, alternating between anomalously warm (El Niño) and cold (La Niña) …
fluctuation on Earth, alternating between anomalously warm (El Niño) and cold (La Niña) …
[HTML][HTML] The Northern Hemisphere extratropical atmospheric circulation response to ENSO: How well do we know it and how do we evaluate models accordingly?
Alexander, MA, I. Blade, M. Newman, J. Lanzante, N.-C. Lau, and JD Scott, 2002: The
atmospheric bridge: The influence of ENSO teleconnections on air–sea interaction over the …
atmospheric bridge: The influence of ENSO teleconnections on air–sea interaction over the …
Recent enhancement of central Pacific El Niño variability relative to last eight centuries
The far-reaching impacts of central Pacific El Niño events on global climate differ
appreciably from those associated with eastern Pacific El Niño events. Central Pacific El …
appreciably from those associated with eastern Pacific El Niño events. Central Pacific El …
[HTML][HTML] The tropospheric pathway of the ENSO–North Atlantic teleconnection
B Jiménez-Esteve, DIV Domeisen - Journal of Climate, 2018 - journals.ametsoc.org
The Tropospheric Pathway of the ENSO–North Atlantic Teleconnection in: Journal of Climate
Volume 31 Issue 11 (2018) Jump to Content Jump to Main Navigation Logo Logo Logo Logo …
Volume 31 Issue 11 (2018) Jump to Content Jump to Main Navigation Logo Logo Logo Logo …
The winter North Pacific teleconnection in response to ENSO and the MJO in operational subseasonal forecasting models is too weak
CI Garfinkel, W Chen, Y Li, C Schwartz… - Journal of …, 2022 - journals.ametsoc.org
Teleconnection patterns associated with the Madden–Julian oscillation (MJO) and El Niño–
Southern Oscillation (ENSO) impact weather and climate phenomena in the Pacific–North …
Southern Oscillation (ENSO) impact weather and climate phenomena in the Pacific–North …
[HTML][HTML] How well do we know ENSO's climate impacts over North America, and how do we evaluate models accordingly?
How Well Do We Know ENSO’s Climate Impacts over North America, and How Do We
Evaluate Models Accordingly? in: Journal of Climate Volume 31 Issue 13 (2018) Jump to …
Evaluate Models Accordingly? in: Journal of Climate Volume 31 Issue 13 (2018) Jump to …
Seasonal predictability over Europe arising from El Niño and stratospheric variability in the MPI-ESM seasonal prediction system
DIV Domeisen, AH Butler, K Fröhlich… - Journal of …, 2015 - journals.ametsoc.org
Predictability on seasonal time scales over the North Atlantic–Europe region is assessed
using a seasonal prediction system based on an initialized version of the Max Planck …
using a seasonal prediction system based on an initialized version of the Max Planck …
Impact of the MJO on the boreal winter extratropical circulation
CI Garfinkel, JJ Benedict… - Geophysical Research …, 2014 - Wiley Online Library
The effect of the Madden‐Julian Oscillation (MJO) on the Northern Hemisphere wintertime
stratospheric polar vortex is evaluated using a meteorological reanalysis data set and a …
stratospheric polar vortex is evaluated using a meteorological reanalysis data set and a …
The climate‐system historical forecast project: Do stratosphere‐resolving models make better seasonal climate predictions in boreal winter?
Using an international, multi‐model suite of historical forecasts from the World Climate
Research Programme (WCRP) Climate‐system Historical Forecast Project (CHFP), we …
Research Programme (WCRP) Climate‐system Historical Forecast Project (CHFP), we …