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 …

Recent paleoclimate proxy reconstructions show that tropical surface temperatures may
have been as high as 35°–40° C in the Early Cenozoic. Here, we study the tropical …

It is argued that deep atmospheric convection might occur during winter in ice‐free high‐
latitude oceans, and that the surface radiative warming effects of the clouds and water vapor …

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 …

Tropical Cyclones Downscaled from Simulations with Very High Carbon Dioxide Levels in:
Journal of Climate Volume 30 Issue 2 (2017) Jump to Content Jump to Main Navigation …

Stratosphere circulation is important to interpret abundances of photochemically produced
compounds like ozone which we aim to observe to assess habitability of exoplanets. We …

Climate models underestimate the magnitude of Arctic warming in past warm climates, like
the early Cretaceous and Paleogene periods, implying that certain physical processes might …

The tropical overturning circulation is examined in a moist aquaplanet general circulation
model forced using a non‐interactive sea‐surface temperature (SST) distribution that varies …

A convective cloud feedback on extratropical surface temperatures is identified in a zonally
averaged two‐level atmospheric model. The model contains simplified parametrizations for …

The tracks, intensities, and other properties of tropical cyclones downscaled from three
models' simulations of the Last Glacial Maximum (LGM) are analyzed and compared to …