Recent hiatus caused by decadal shift in Indo-Pacific heating

Looking for the missing heat Global warming apparently slowed, or even stopped, during the first decade of the 21st century. This pause is commonly called the “hiatus.” We know, however, that Earth's climate system is accumulating excess solar energy owing to the build-up of greenhouse gases in the atmosphere. Where, then, has this energy gone if not into the air? Nieves et al. find that over this period, the surface Pacific Ocean has cooled but the upper Indian and Southern Oceans have warmed. Thus, the decade-long hiatus that began in 2003 would appear to be the result of a redistribution of heat within the ocean, rather than a change in the whole-Earth warming rate. Science, this issue p. 532 Shifting ocean heat distributions slowed global warming. Recent modeling studies have proposed different scenarios to explain the slowdown in surface temperature warming in the most recent decade. Some of these studies seem to support the idea of internal variability and/or rearrangement of heat between the surface and the ocean interior. Others suggest that radiative forcing might also play a role. Our examination of observational data over the past two decades shows some significant differences when compared to model results from reanalyses and provides the most definitive explanation of how the heat was redistributed. We find that cooling in the top 100-meter layer of the Pacific Ocean was mainly compensated for by warming in the 100- to 300-meter layer of the Indian and Pacific Oceans in the past decade since 2003.

[1]  Wonsun Park,et al.  Pacific origin of the abrupt increase in Indian Ocean heat content during the warming hiatus , 2015 .

[2]  Dean Roemmich,et al.  Unabated planetary warming and its ocean structure since 2006 , 2015 .

[3]  M. Balmaseda,et al.  Surface warming hiatus caused by increased heat uptake across multiple ocean basins , 2014 .

[4]  D. Chambers,et al.  Relative contributions of ocean mass and deep steric changes to sea level rise between 1993 and 2013 , 2014 .

[5]  R. Knutti,et al.  Natural variability, radiative forcing and climate response in the recent hiatus reconciled , 2014 .

[6]  K. Tung,et al.  Varying planetary heat sink led to global-warming slowdown and acceleration , 2014, Science.

[7]  Lijing Cheng,et al.  Time, Probe Type, and Temperature Variable Bias Corrections to Historical Expendable Bathythermograph Observations , 2014 .

[8]  Agus Santoso,et al.  Recent intensification of wind-driven circulation in the Pacific and the ongoing warming hiatus , 2014 .

[9]  J. Sprintall,et al.  The Indonesian Throughflow response to Indo‐Pacific climate variability , 2014 .

[10]  J. Sprintall,et al.  Pacific‐to‐Indian Ocean connectivity: Tasman leakage, Indonesian Throughflow, and the role of ENSO , 2014 .

[11]  Kevin E. Trenberth,et al.  An apparent hiatus in global warming? , 2013 .

[12]  Yu Kosaka,et al.  Recent global-warming hiatus tied to equatorial Pacific surface cooling , 2013, Nature.

[13]  John Abraham,et al.  A review of global ocean temperature observations: Implications for ocean heat content estimates and climate change , 2013, Reviews of Geophysics.

[14]  M. Balmaseda,et al.  Evaluation of the ECMWF ocean reanalysis system ORAS4 , 2013 .

[15]  Kevin E. Trenberth,et al.  Distinctive climate signals in reanalysis of global ocean heat content , 2013 .

[16]  S. Levitus,et al.  World ocean heat content and thermosteric sea level change (0–2000 m), 1955–2010 , 2012 .

[17]  J. Gregory,et al.  Revisiting the Earth's sea‐level and energy budgets from 1961 to 2008 , 2011, Geophysical Research Letters.

[18]  D. Roemmich,et al.  The global ocean imprint of ENSO , 2011 .

[19]  C. Böning,et al.  Contribution of Pacific wind stress to multi‐decadal variations in upper‐ocean heat content and sea level in the tropical south Indian Ocean , 2011 .

[20]  Sheng-Ping Wang,et al.  Validation of the Global Ocean Data Assimilation System (GODAS) data in the NOAA National Centre for Environmental System (NCEP) by theory, comparative studies, applications and sea truth , 2011 .

[21]  Lee-Lueng Fu,et al.  Combining altimeter and subsurface float data to estimate the time‐averaged circulation in the upper ocean , 2008 .

[22]  G. Johnson,et al.  Estimating Annual Global Upper-Ocean Heat Content Anomalies despite Irregular In Situ Ocean Sampling* , 2008 .

[23]  J. Carton,et al.  A Reanalysis of Ocean Climate Using Simple Ocean Data Assimilation (SODA) , 2008 .

[24]  Satoshi Sugimoto,et al.  Objective analyses of sea‐surface temperature and marine meteorological variables for the 20th century using ICOADS and the Kobe Collection , 2005 .

[25]  J. Willis,et al.  Interannual variability in upper ocean heat content, temperature, and thermosteric expansion on global scales , 2004 .

[26]  J. Willis,et al.  Combining altimetric height with broadscale profile data to estimate steric height, heat storage, subsurface temperature, and sea-surface temperature variability , 2003 .

[27]  Thomas M. Smith,et al.  An Improved In Situ and Satellite SST Analysis for Climate , 2002 .

[28]  Gilles Reverdin,et al.  Global high-resolution mapping of ocean circulation from TOPEX/Poseidon and ERS-1 and -2 , 2000 .

[29]  K. Shine,et al.  Intergovernmental panel on Climate change (IPCC),in encyclopedia of Enviroment and society,Vol.3 , 2007 .