Observational and Model Estimates of Cloud Amount Feedback over the Indian and Pacific Oceans

AbstractConstraining intermodel spread in cloud feedback with observations is problematic because available cloud datasets are affected by spurious behavior in long-term variability. This problem is addressed by examining cloud amount in three independent ship-based [Extended Edited Cloud Reports Archive (EECRA)] and satellite-based [International Satellite Cloud Climatology Project (ISCCP) and Advanced Very High Resolution Radiometer Pathfinder Atmosphere–Extended (PATMOS-X)] observational datasets, and models from phase 5 of the Coupled Model Intercomparison Project (CMIP5). The three observational datasets show consistent cloud variability in the overlapping years of coverage (1984–2007). The long-term cloud amount change from 1954 to 2005 in ship-based observations shares many of the same features with the multimodel mean cloud amount change of 42 CMIP5 historical simulations, although the magnitude of the multimodel mean is smaller. The radiative impact of cloud changes is estimated by computing an o...

[1]  Corinne Le Quéré,et al.  Climate Change 2013: The Physical Science Basis , 2013 .

[2]  J. Norris,et al.  Observational Evidence That Enhanced Subsidence Reduces Subtropical Marine Boundary Layer Cloudiness , 2013 .

[3]  G. Tselioudis,et al.  The ozone hole indirect effect: Cloud‐radiative anomalies accompanying the poleward shift of the eddy‐driven jet in the Southern Hemisphere , 2013 .

[4]  M. Zelinka,et al.  An Analysis of the Short-Term Cloud Feedback Using MODIS Data , 2013 .

[5]  A. Evan,et al.  The Modification of Sea Surface Temperature Anomaly Linear Damping Time Scales by Stratocumulus Clouds , 2013 .

[6]  S. Bony,et al.  Interpretation of the positive low-cloud feedback predicted by a climate model under global warming , 2013, Climate Dynamics.

[7]  K. Taylor,et al.  Contributions of Different Cloud Types to Feedbacks and Rapid Adjustments in CMIP5 , 2012 .

[8]  C. Deser,et al.  Slowdown of the Walker circulation driven by tropical Indo-Pacific warming , 2012, Nature.

[9]  S. Bony,et al.  The ‘too few, too bright’ tropical low‐cloud problem in CMIP5 models , 2012 .

[10]  S. Klein,et al.  Are climate model simulations of clouds improving? An evaluation using the ISCCP simulator , 2012 .

[11]  Mark D. Zelinka,et al.  Computing and Partitioning Cloud Feedbacks Using Cloud Property Histograms. Part II: Attribution to Changes in Cloud Amount, Altitude, and Optical Depth , 2012 .

[12]  S. Sherwood,et al.  Recent Northern Hemisphere tropical expansion primarily driven by black carbon and tropospheric ozone , 2012, Nature.

[13]  Karl E. Taylor,et al.  An overview of CMIP5 and the experiment design , 2012 .

[14]  Nicolas Bellouin,et al.  Aerosols implicated as a prime driver of twentieth-century North Atlantic climate variability. , 2012, Nature.

[15]  Robert Pincus,et al.  Reconciling Simulated and Observed Views of Clouds: MODIS, ISCCP, and the Limits of Instrument Simulators in Climate Models , 2011 .

[16]  Stephen A. Klein,et al.  Computing and Partitioning Cloud Feedbacks Using Cloud Property Histograms. Part I: Cloud Radiative Kernels , 2012 .

[17]  Stephen G. Warren,et al.  Variations in Cloud Cover and Cloud Types over the Ocean from Surface Observations, 1954-2008 , 2011 .

[18]  B. Stevens,et al.  On the Factors Modulating the Stratocumulus to Cumulus Transitions , 2011 .

[19]  G. Vecchi,et al.  The response of the Walker circulation to Last Glacial Maximum forcing: Implications for detection in proxies , 2011 .

[20]  Elizabeth C. Kent,et al.  ICOADS Release 2.5: extensions and enhancements to the surface marine meteorological archive , 2011 .

[21]  G. Vecchi,et al.  The vertical distribution of cloud feedback in coupled ocean‐atmosphere models , 2011 .

[22]  J. Rutllant,et al.  The Coastal Boundary Layer at the Eastern Margin of the Southeast Pacific (23.4°S, 70.4°W): Cloudiness-Conditioned Climatology , 2011 .

[23]  C. Deser,et al.  Uncertainty in climate change projections: the role of internal variability , 2012, Climate Dynamics.

[24]  Mark D. Zelinka,et al.  The observed sensitivity of high clouds to mean surface temperature anomalies in the tropics , 2010 .

[25]  R. Marchand,et al.  There are notable differences in the joint histograms of cloud top height and optical depth being produced from the Moderate Resolution Imaging Spectroradiometer ( MODIS ) and the Multiangle Imaging Spectro ‐ Radiometer , 2010 .

[26]  Mark D. Zelinka,et al.  Why is longwave cloud feedback positive , 2010 .

[27]  J. Norris,et al.  Assessing the Impact of Meteorological History on Subtropical Cloud Fraction , 2010 .

[28]  C. Deser,et al.  Twentieth century tropical sea surface temperature trends revisited , 2010 .

[29]  C. Deser,et al.  Global warming pattern formation: sea surface temperature and rainfall. , 2010 .

[30]  G. Vecchi,et al.  Climate Response of the Equatorial Pacific to Global Warming , 2009 .

[31]  Robert Burgman,et al.  Observational and Model Evidence for Positive Low-Level Cloud Feedback , 2009, Science.

[32]  K. Trenberth,et al.  Global warming due to increasing absorbed solar radiation , 2009 .

[33]  R. Seager,et al.  Forced and Internal Twentieth-Century SST Trends in the North Atlantic* , 2009 .

[34]  M. Falvey,et al.  Regional cooling in a warming world: Recent temperature trends in the southeast Pacific and along the west coast of subtropical South America (1979–2006) , 2009 .

[35]  David R. Doelling,et al.  Toward Optimal Closure of the Earth's Top-of-Atmosphere Radiation Budget , 2009 .

[36]  Sandrine Bony,et al.  An Assessment of the Primary Sources of Spread of Global Warming Estimates from Coupled Atmosphere–Ocean Models , 2008 .

[37]  C. Bretherton,et al.  Aquaplanets, Climate Sensitivity, and Low Clouds , 2008 .

[38]  Brian J. Soden,et al.  Quantifying Climate Feedbacks Using Radiative Kernels , 2008 .

[39]  K. Taylor,et al.  Estimating shortwave radiative forcing and response in climate models , 2007 .

[40]  G. Vecchi,et al.  Global Warming and the Weakening of the Tropical Circulation , 2007 .

[41]  G. Vecchi,et al.  Increased tropical Atlantic wind shear in model projections of global warming , 2007 .

[42]  B. Stevens,et al.  On the Structure of the Lower Troposphere in the Summertime Stratocumulus Regime of the Northeast Pacific , 2007 .

[43]  A. Evan,et al.  Arguments against a physical long‐term trend in global ISCCP cloud amounts , 2007 .

[44]  C. Bretherton,et al.  On the Relationship between Stratiform Low Cloud Cover and Lower-Tropospheric Stability , 2006 .

[45]  S. Bony,et al.  How Well Do We Understand and Evaluate Climate Change Feedback Processes , 2006 .

[46]  B. Soden,et al.  An Assessment of Climate Feedbacks in Coupled Ocean–Atmosphere Models , 2006 .

[47]  G. Vecchi,et al.  Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing , 2006, Nature.

[48]  Johannes Quaas,et al.  Global mean cloud feedbacks in idealized climate change experiments , 2006 .

[49]  I. Musat,et al.  On the contribution of local feedback mechanisms to the range of climate sensitivity in two GCM ensembles , 2006 .

[50]  R. Reynolds,et al.  Early Ship Observational Data and Icoads , 2005 .

[51]  S. Bony,et al.  Marine boundary layer clouds at the heart of tropical cloud feedback uncertainties in climate models , 2005 .

[52]  Taneil Uttal,et al.  Daytime Global Cloud Typing from AVHRR and VIIRS: Algorithm Description, Validation, and Comparisons , 2005 .

[53]  J. Norris Multidecadal Changes in Near-Global Cloud Cover and Estimated Cloud Cover Radiative Forcing , 2005 .

[54]  G. Stephens Cloud Feedbacks in the Climate System: A Critical Review , 2005 .

[55]  C. Bretherton,et al.  Boundary Layer Depth, Entrainment, and Decoupling in the Cloud-Capped Subtropical and Tropical Marine Boundary Layer , 2004 .

[56]  C. Deser,et al.  Pacific Interdecadal Climate Variability: Linkages between the Tropics and the North Pacific during Boreal Winter since 1900 , 2004 .

[57]  S. Bony,et al.  On dynamic and thermodynamic components of cloud changes , 2004 .

[58]  Elizabeth C. Kent,et al.  Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century , 2003 .

[59]  Andrew K. Heidinger,et al.  The Advanced Very High Resolution Radiometer Pathfinder Atmosphere (PATMOS) Climate Dataset: A Resource for Climate Research , 2003 .

[60]  Dennis L. Hartmann,et al.  An important constraint on tropical cloud ‐ climate feedback , 2002 .

[61]  W. Rossow,et al.  Advances in understanding clouds from ISCCP , 1999 .

[62]  C. J. Hahn,et al.  Extended Edited Synoptic Cloud Reports from Ships and Land Stations Over the Globe, 1952-1996 , 1999 .

[63]  J. Norris On Trends and Possible Artifacts in Global Ocean Cloud Cover between 1952 and 1995 , 1999 .

[64]  J. Norris Low Cloud Type over the Ocean from Surface Observations. Part II: Geographical and Seasonal Variations , 1998 .

[65]  Ronald L. Miller Tropical Thermostats and Low Cloud Cover , 1997 .

[66]  C. Bretherton,et al.  Moisture Transport, Lower-Tropospheric Stability, and Decoupling of Cloud-Topped Boundary Layers , 1997 .

[67]  C. Bretherton,et al.  The Atlantic Stratocumulus Transition Experiment - ASTEX , 1995 .

[68]  S. Klein,et al.  On the Relationships among Low-Cloud Structure, Sea Surface Temperature, and Atmospheric Circulation in the Summertime Northeast Pacific , 1995 .

[69]  S. Klein,et al.  The Seasonal Cycle of Low Stratiform Clouds , 1993 .