A distributional regression network acts as a backward operator to produce uncertainty-quantified, multivariate Gaussian retrievals of cloud properties from six solar channels for data assimilation.
Title resolution pending
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
A thermodynamic uncertainty relation imposes an entropy-based constraint on the seasonal phase locking of ENSO variance in a linear stochastic recharge oscillator model.
LES of a real campus finds shielding controls individual building drag, quantified by upstream fetch ratio L_s/H_s and relative height ratio H_s/H.
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
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Using Distributional Regression Networks to Retrieve Cloud Properties from Solar Satellite Channels for Data Assimilation
A distributional regression network acts as a backward operator to produce uncertainty-quantified, multivariate Gaussian retrievals of cloud properties from six solar channels for data assimilation.
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A Stochastic-Thermodynamic Constraint on the Seasonal Phase Locking of the El Ni\~no-Southern Oscillation
A thermodynamic uncertainty relation imposes an entropy-based constraint on the seasonal phase locking of ENSO variance in a linear stochastic recharge oscillator model.
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Building drag and shielding in a realistic urban environment
LES of a real campus finds shielding controls individual building drag, quantified by upstream fetch ratio L_s/H_s and relative height ratio H_s/H.
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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.