Results 51 to 60 of about 2,949 (160)

Decomposing Cloud Radiative Feedbacks by Cloud-Top Phase [PDF]

open access: yesJournal of Climate
Changes in cloud scattering properties and emissivity that arise from atmospheric warming cause substantial radiative feedbacks in model projections of anthropogenic climate change, and the relative importance of the underlying mechanisms is poorly understood.
Casey J. Wall   +11 more
openaire   +1 more source

Stellar feedback effects on the mass distribution of clouds and cloud complexes

open access: yesAstronomy & Astrophysics
Context . Galaxy evolution is sensitive to how stars inject feedback into their surroundings. In particular, the stellar feedback from star clusters strongly affects gas motions and, consequently, the baryonic cycle. More massive clusters have stronger effects.
Luanna Veroneze Quinalha   +2 more
openaire   +2 more sources

Mechanisms of marine low cloud sensitivity to idealized climate perturbations: A single‐LES exploration extending the CGILS cases

open access: yesJournal of Advances in Modeling Earth Systems, 2013
Climate change sensitivities of subtropical cloud‐topped marine boundary layers are analyzed using large‐eddy simulation (LES) of three CGILS cases of well‐mixed stratocumulus, cumulus under stratocumulus, and shallow cumulus cloud regimes, respectively.
Christopher S. Bretherton   +2 more
doaj   +1 more source

Mid-latitude clouds contribute to Arctic amplification via interactions with other climate feedbacks

open access: yesEnvironmental Research: Climate
Traditional feedback analyses, which assume that individual climate feedback mechanisms act independently and add linearly, suggest that clouds do not contribute to Arctic amplification.
David B Bonan   +3 more
doaj   +1 more source

Climate warming could weaken aerosol-cloud interactions in subtropical marine stratocumulus

open access: yesnpj Climate and Atmospheric Science
Radiative effects of aerosol-cloud interactions constitute the most uncertain climate forcing of the Earth system. To understand how these interactions may change with climate, we conduct 3-day-long large-eddy simulations of a stratocumulus-to-cumulus ...
Hongwei Sun   +5 more
doaj   +1 more source

Coupling between lower‐tropospheric convective mixing and low‐level clouds: Physical mechanisms and dependence on convection scheme

open access: yesJournal of Advances in Modeling Earth Systems, 2016
Several studies have pointed out the dependence of low‐cloud feedbacks on the strength of the lower‐tropospheric convective mixing. By analyzing a series of single‐column model experiments run by a climate model using two different convective ...
Jessica Vial   +3 more
doaj   +1 more source

Relevant Clouds: Leveraging Relevance Feedback to Build Tag Clouds for Image Search [PDF]

open access: yes, 2013
Work supported by EU FP7/2007-2013 under grant agreements 600707 (tranScriptorium) and 287576 (CasMaCat), and by the STraDA project (TIN2012-37475-C02-01).
Luis A. Leiva   +2 more
openaire   +2 more sources

The Single Column Atmosphere Model Version 6 (SCAM6): Not a Scam but a Tool for Model Evaluation and Development

open access: yesJournal of Advances in Modeling Earth Systems, 2019
The Single Column Atmosphere Model (SCAM) is a single column model version of the Community Atmosphere Model (CAM). Here we describe the functionality and features of SCAM6, available as part of CAM6 in the Community Earth System Model, version 2 (CESM2).
A. Gettelman   +6 more
doaj   +1 more source

Evaporative Resistance is of Equal Importance as Surface Albedo in High‐Latitude Surface Temperatures Due to Cloud Feedbacks

open access: yesGeophysical Research Letters, 2020
Arctic vegetation is known to influence Arctic surface temperatures through albedo. However, it is less clear how plant evaporative resistance and albedo independently influence surface climate at high latitudes.
Jinhyuk E. Kim   +4 more
doaj   +1 more source

Parametric Sensitivity of Hemispheric Albedo Symmetry Weakly Constrains Shortwave Cloud Radiative Feedbacks in the Community Atmosphere Model Version 6

open access: yesGeophysical Research Letters
Earth's albedo is symmetric between the northern and southern hemispheres (NH and SH, respectively) because SH clouds compensate for higher NH clear‐sky albedo, a feature that climate models have difficulty capturing.
Aiden Jönsson   +4 more
doaj   +1 more source

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