Atmosphere functions as steam engine with global power 4.4±0.9 W/m² from water cycle, matching total atmospheric power 4.3±0.6 W/m² and explaining condensation-driven dynamics via precipitation.
The asymmetric boundary layer flow under a translating hurricane.Journal of the Atmospheric Sciences, 40(8):1984–1998
4 Pith papers cite this work. Polarity classification is still indexing.
4
Pith papers citing it
fields
physics.ao-ph 4years
2026 4verdicts
UNVERDICTED 4representative citing papers
Reconstruction of global 1.5 km resolution 10 m vector winds in tropical cyclone inner cores from sparse CYGNSS scalar observations using generalized score-based diffusion assimilation plus three TC boundary-layer constraints.
A tornado outbreak with simultaneous tornadic supercells occurred in the Philippines within an easterly severe weather regime, documented as the first known instance there.
Atmospheric response to Gulf Stream front shifts is strongly resolution-dependent below 50 km and NAO leads GSF shifts by 2-3 years only during 1972-2018 with non-stationary behavior linked to oceanic circulation and Rossby waves.
citing papers explorer
-
Atmosphere as a steam engine
Atmosphere functions as steam engine with global power 4.4±0.9 W/m² from water cycle, matching total atmospheric power 4.3±0.6 W/m² and explaining condensation-driven dynamics via precipitation.
-
Global kilometre-scale tropical cyclone inner-core vector winds from sparse scalar CYGNSS observations
Reconstruction of global 1.5 km resolution 10 m vector winds in tropical cyclone inner cores from sparse CYGNSS scalar observations using generalized score-based diffusion assimilation plus three TC boundary-layer constraints.
-
Localized Tornado Outbreak at the Upstream of a Tropical Easterly Wave in Camarines Norte, Philippines (13 September 2025)
A tornado outbreak with simultaneous tornadic supercells occurred in the Philippines within an easterly severe weather regime, documented as the first known instance there.
-
Ocean-atmosphere interaction at the Gulf Stream sea surface temperature front: variability and impacts on midlatitude atmospheric circulation
Atmospheric response to Gulf Stream front shifts is strongly resolution-dependent below 50 km and NAO leads GSF shifts by 2-3 years only during 1972-2018 with non-stationary behavior linked to oceanic circulation and Rossby waves.