The response of tropical high clouds to surface warming and their radiative feedbacks are
uncertain. For example, it is uncertain whether their coverage will contract or expand in …

The effect of warming on severe convective storm potential is commonly explained in terms
of changes in vertically integrated (“bulk”) environmental parameters, such as CAPE and 0 …

This work develops a theoretical model for steady thermodynamic and kinematic profiles for
severe convective storm environments, building off the two-layer static energy framework …

Cloud-radiative heating (CRH) within the atmosphere and its changes with warming affect
the large-scale atmospheric winds in a myriad of ways, such that reliable predictions and …

The response of upper tropospheric clouds and relative humidity (RH) to warming is
important to the overall sensitivity of the Earth to increasing greenhouse gas concentrations …

The extratropics are the cloudiest region on Earth. Changes in clouds in this region in
response to warming have the potential to substantially affect global mean cloud feedback …

Axisymmetric Hadley Cell Theory with a Fixed Tropopause Temperature Rather than Height in:
Journal of the Atmospheric Sciences Volume 77 Issue 4 (2020) Jump to Content Jump to Main …

The ways in which clouds, circulation, and climate sensitivity interact are grand challenges
of climate science. All of these phenomena depend on water vapor's condensable nature …

Cloud-radiative heating (CRH) within the atmosphere and its changes with warming affect
the large-scale atmospheric wind patterns in a myriad of ways, such that reliable predictions …

This work develops a theoretical model for steady thermodynamic and kinematic profiles for
severe convective storm environments, building off of the two-layer static energy framework …