Results 31 to 40 of about 1,625 (108)
Clouds, Circulation, and Climate Sensitivity in a Radiative‐Convective Equilibrium Channel Model
Tropical cloud and circulation changes are large sources of uncertainty in future climate change. This problem owes partly to the scale separation between large‐scale tropical dynamics ( ∼104 km) and convective dynamics ( ∼1 km), which generally requires
Timothy W. Cronin, Allison A. Wing
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Coarse, intermediate and high resolution numerical simulations of the transition of a tropical wave critical layer to a tropical storm [PDF]
Recent work has hypothesized that tropical cyclones in the deep Atlantic and eastern Pacific basins develop from within the cyclonic Kelvin cat's eye of a tropical easterly wave critical layer located equatorward of the easterly jet axis.
M. T. Montgomery +2 more
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Quantifying Convective Aggregation Using the Tropical Moist Margin's Length
On small scales, the tropical atmosphere tends to be either moist or very dry. This defines two states that, on large scales, are separated by a sharp margin, well identified by the antimode of the bimodal tropical column water vapor distribution ...
Tom Beucler +2 more
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In a modeled environment of rotating radiative‐convective equilibrium (RCE), convective self‐aggregation may take the form of spontaneous tropical cyclogenesis. We investigate the processes leading to tropical cyclogenesis in idealized simulations with a
Jacob D. Carstens, Allison A. Wing
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Terrestrial nanoplastics (NPs) pose a serious threat to agricultural food production systems due to the potential harm of soil-born micro- and macroorganisms that promote soil fertility and ability of NPs to adsorb onto and penetrate into vegetables and ...
Anton F Astner +6 more
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Tipping to an Aggregated State by Mesoscale Convective Systems
Radiative‐convective equilibrium simulations were suggested to resist self‐aggregation within a linearly stable regime at low surface temperatures. Recent numerical work shows that this linearly stable regime can rapidly transition to an aggregated state
I. L. Kruse, R. Fiévet, J. O. Haerter
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We have addressed convective self‐aggregation (CSA) in steady and oscillating sea surface temperature (SST) and solar radiation (SOLIN) cloud‐resolving model simulations in a non‐rotating radiative‐convective equilibrium (RCE) framework.
Bidyut Bikash Goswami +2 more
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Deep convection over tropical oceans often appears intensified at the edge of convectively active regions, both in idealized studies and in observations.
J. M. Windmiller, C. Hohenegger
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Circling in on Convective Self-Aggregation. [PDF]
Nissen SB, Haerter JO.
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The elimination of rain evaporation in the planetary boundary layer (PBL) has been found to lead to convective self‐aggregation (CSA) even without radiative feedback, but the precise mechanisms underlying this phenomenon remain unclear.
Y.‐L. Hwong, C. J. Muller
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