Moist heat stress on a hotter Earth
As the world overheats—potentially to conditions warmer than during the three million years
over which modern humans evolved—suffering from heat stress will become widespread …
over which modern humans evolved—suffering from heat stress will become widespread …
Water vapor and the dynamics of climate changes
T Schneider, PA O'Gorman… - Reviews of Geophysics, 2010 - Wiley Online Library
Water vapor is not only Earth's dominant greenhouse gas. Through the release of latent heat
when it condenses, it also plays an active role in dynamic processes that shape the global …
when it condenses, it also plays an active role in dynamic processes that shape the global …
Fast upper-level jet stream winds get faster under climate change
TA Shaw, O Miyawaki - Nature Climate Change, 2024 - nature.com
Earth's upper-level jet streams influence the speed and direction of travel of weather
systems and commercial aircraft, and are linked to severe weather occurrence. Climate …
systems and commercial aircraft, and are linked to severe weather occurrence. Climate …
An upper bound for extreme temperatures over midlatitude land
Heatwaves damage societies worldwide and are intensifying with global warming. Several
mechanistic drivers of heatwaves, such as atmospheric blocking and soil moisture …
mechanistic drivers of heatwaves, such as atmospheric blocking and soil moisture …
Non‐local parameterization of atmospheric subgrid processes with neural networks
Subgrid processes in global climate models are represented by parameterizations which are
a major source of uncertainties in simulations of climate. In recent years, it has been …
a major source of uncertainties in simulations of climate. In recent years, it has been …
The global atmospheric circulation on moist isentropes
The global atmospheric circulation transports energy from the equatorial regions to higher
latitudes through a poleward flow of high-energy and-entropy parcels and an equatorward …
latitudes through a poleward flow of high-energy and-entropy parcels and an equatorward …
[HTML][HTML] Energy of midlatitude transient eddies in idealized simulations of changed climates
PA O'Gorman, T Schneider - Journal of Climate, 2008 - journals.ametsoc.org
Energy of Midlatitude Transient Eddies in Idealized Simulations of Changed Climates in:
Journal of Climate Volume 21 Issue 22 (2008) Jump to Content Jump to Main Navigation …
Journal of Climate Volume 21 Issue 22 (2008) Jump to Content Jump to Main Navigation …
[HTML][HTML] The global atmospheric circulation in moist isentropic coordinates
The Global Atmospheric Circulation in Moist Isentropic Coordinates in: Journal of Climate
Volume 23 Issue 11 (2010) Jump to Content Jump to Main Navigation Logo Logo Logo Logo …
Volume 23 Issue 11 (2010) Jump to Content Jump to Main Navigation Logo Logo Logo Logo …
[HTML][HTML] Baroclinic eddies and the extent of the Hadley circulation: An idealized GCM study
XJ Levine, T Schneider - Journal of the Atmospheric Sciences, 2015 - journals.ametsoc.org
Baroclinic Eddies and the Extent of the Hadley Circulation: An Idealized GCM Study in: Journal
of the Atmospheric Sciences Volume 72 Issue 7 (2015) Jump to Content Jump to Main …
of the Atmospheric Sciences Volume 72 Issue 7 (2015) Jump to Content Jump to Main …
[HTML][HTML] Ocean heat transport and water vapor greenhouse in a warm equable climate: A new look at the low gradient paradox
BEJ Rose, D Ferreira - Journal of Climate, 2012 - journals.ametsoc.org
Ocean Heat Transport and Water Vapor Greenhouse in a Warm Equable Climate: A New
Look at the Low Gradient Paradox in: Journal of Climate Volume 26 Issue 6 (2012) Jump to …
Look at the Low Gradient Paradox in: Journal of Climate Volume 26 Issue 6 (2012) Jump to …