Recent progress is reviewed in the understanding of convective interaction with water vapor and changes associated with water vapor in warmer climates. Progress includes new …
DA Randall, RA Wood, S Bony, R Colman… - Climate change 2007 …, 2007 - pure.mpg.de
This chapter assesses the capacity of the global climate models used elsewhere in this report for projecting future climate change. Confidence in model estimates of future climate …
S Bony, R Colman, VM Kattsov, RP Allan… - Journal of …, 2006 - journals.ametsoc.org
How Well Do We Understand and Evaluate Climate Change Feedback Processes? in: Journal of Climate Volume 19 Issue 15 (2006) Jump to Content Jump to Main Navigation …
AE Dessler, MR Schoeberl, T Wang… - Proceedings of the …, 2013 - National Acad Sciences
We show here that stratospheric water vapor variations play an important role in the evolution of our climate. This comes from analysis of observations showing that stratospheric …
Although in principle transition metals can form bonds with six shared electron pairs, only quadruply bonded compounds can be isolated as stable species at room temperature. Here …
R Colman, BJ Soden - Reviews of Modern Physics, 2021 - APS
Water vapor is a greenhouse gas that dominates Earth's terrestrial radiation absorption. As the planetary temperature warms, forced by increasing CO 2 and other greenhouse gases …
MD Zelinka, DL Hartmann - Journal of Geophysical Research …, 2010 - Wiley Online Library
Longwave cloud feedback is systematically positive and nearly the same magnitude across all global climate models used in the Intergovernmental Panel on Climate Change Fourth …
DM Romps - Journal of Climate, 2014 - journals.ametsoc.org
An analytical model is derived for tropical relative humidity using only the Clausius– Clapeyron relation, hydrostatic balance, and a bulk-plume water budget. This theory is …
AE Dessler, Z Zhang, P Yang - Geophysical Research Letters, 2008 - Wiley Online Library
Between 2003 and 2008, the global‐average surface temperature of the Earth varied by 0.6° C. We analyze here the response of tropospheric water vapor to these variations. Height …