Articles | Volume 11, issue 17
https://doi.org/10.5194/acp-11-9053-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-11-9053-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
05 Sep 2011
Research article |
| 05 Sep 2011
On the relationship between low cloud variability and lower tropospheric stability in the Southeast Pacific
F. Sun
Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, Los Angeles, CA, 90095, USA
A. Hall
Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, Los Angeles, CA, 90095, USA
X. Qu
Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, Los Angeles, CA, 90095, USA
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Cited
17 citations as recorded by crossref.
- The northward march of summer low cloudiness along the California coast R. Clemesha et al. 10.1002/2015GL067081
- Observational Evidence That Enhanced Subsidence Reduces Subtropical Marine Boundary Layer Cloudiness T. Myers & J. Norris 10.1175/JCLI-D-12-00736.1
- On the spread of changes in marine low cloud cover in climate model simulations of the 21st century X. Qu et al. 10.1007/s00382-013-1945-z
- Meteorological observations on the northern Chilean coast during VOCALS-REx J. Rutllant et al. 10.5194/acp-13-3409-2013
- The strength of the tropical inversion and its response to climate change in 18 CMIP5 models X. Qu et al. 10.1007/s00382-014-2441-9
- Intermodel variances of subtropical stratocumulus environments simulated in CMIP5 models A. Noda & M. Satoh 10.1002/2014GL061812
- Global Character of Latent Heat Release in Oceanic Warm Rain Systems E. Nelson & T. L'Ecuyer 10.1002/2017JD027844
- Daily variability of California coastal low cloudiness: A balancing act between stability and subsidence R. Clemesha et al. 10.1002/2017GL073075
- Meteorological and Aerosol Effects on Marine Stratocumulus Z. Li et al. 10.1175/JAS-D-15-0101.1
- Relationships Between Inversion Strength, Lower‐Tropospheric Moistening, and Low‐Cloud Fraction in the Subtropical Southeast Pacific Derived From Stable Isotopologues of Water Vapor J. Galewsky 10.1029/2018GL078953
- Evaluating Marine Stratocumulus Clouds in the CNRM‐CM6‐1 Model Using Short‐Term Hindcasts F. Brient et al. 10.1029/2018MS001461
- Ocean–Cloud–Atmosphere–Land Interactions in the Southeastern Pacific: The VOCALS Program C. Mechoso et al. 10.1175/BAMS-D-11-00246.1
- Uncertainty Quantification and Bayesian Inference of Cloud Parameterization in the NCAR Single Column Community Atmosphere Model (SCAM6) R. Pathak et al. 10.3389/fclim.2021.670740
- Regional variabilities of rainfall and convective parameters during the summer monsoon period: their linkage with El Niño Southern Oscillation P. Hrudya et al. 10.1007/s00703-021-00802-4
- Day-night changes in the altitude distribution, physical properties and radiative impact of low-altitude clouds over the stratocumulus-dominated subtropical oceans A. Gupta et al. 10.1016/j.jastp.2017.06.021
- The Cloud_cci simulator v1.0 for the Cloud_cci climate data record and its application to a global and a regional climate model S. Eliasson et al. 10.5194/gmd-12-829-2019
- The representation of dry-season low-level clouds over Western Equatorial Africa in reanalyses and historical CMIP6 simulations P. Camberlin et al. 10.1007/s00382-023-06714-w
17 citations as recorded by crossref.
- The northward march of summer low cloudiness along the California coast R. Clemesha et al. 10.1002/2015GL067081
- Observational Evidence That Enhanced Subsidence Reduces Subtropical Marine Boundary Layer Cloudiness T. Myers & J. Norris 10.1175/JCLI-D-12-00736.1
- On the spread of changes in marine low cloud cover in climate model simulations of the 21st century X. Qu et al. 10.1007/s00382-013-1945-z
- Meteorological observations on the northern Chilean coast during VOCALS-REx J. Rutllant et al. 10.5194/acp-13-3409-2013
- The strength of the tropical inversion and its response to climate change in 18 CMIP5 models X. Qu et al. 10.1007/s00382-014-2441-9
- Intermodel variances of subtropical stratocumulus environments simulated in CMIP5 models A. Noda & M. Satoh 10.1002/2014GL061812
- Global Character of Latent Heat Release in Oceanic Warm Rain Systems E. Nelson & T. L'Ecuyer 10.1002/2017JD027844
- Daily variability of California coastal low cloudiness: A balancing act between stability and subsidence R. Clemesha et al. 10.1002/2017GL073075
- Meteorological and Aerosol Effects on Marine Stratocumulus Z. Li et al. 10.1175/JAS-D-15-0101.1
- Relationships Between Inversion Strength, Lower‐Tropospheric Moistening, and Low‐Cloud Fraction in the Subtropical Southeast Pacific Derived From Stable Isotopologues of Water Vapor J. Galewsky 10.1029/2018GL078953
- Evaluating Marine Stratocumulus Clouds in the CNRM‐CM6‐1 Model Using Short‐Term Hindcasts F. Brient et al. 10.1029/2018MS001461
- Ocean–Cloud–Atmosphere–Land Interactions in the Southeastern Pacific: The VOCALS Program C. Mechoso et al. 10.1175/BAMS-D-11-00246.1
- Uncertainty Quantification and Bayesian Inference of Cloud Parameterization in the NCAR Single Column Community Atmosphere Model (SCAM6) R. Pathak et al. 10.3389/fclim.2021.670740
- Regional variabilities of rainfall and convective parameters during the summer monsoon period: their linkage with El Niño Southern Oscillation P. Hrudya et al. 10.1007/s00703-021-00802-4
- Day-night changes in the altitude distribution, physical properties and radiative impact of low-altitude clouds over the stratocumulus-dominated subtropical oceans A. Gupta et al. 10.1016/j.jastp.2017.06.021
- The Cloud_cci simulator v1.0 for the Cloud_cci climate data record and its application to a global and a regional climate model S. Eliasson et al. 10.5194/gmd-12-829-2019
- The representation of dry-season low-level clouds over Western Equatorial Africa in reanalyses and historical CMIP6 simulations P. Camberlin et al. 10.1007/s00382-023-06714-w
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