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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-13421-2011</article-id>
<title-group>
<article-title>Earth&apos;s energy imbalance and implications</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hansen</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sato</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kharecha</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>von Schuckmann</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>NASA Goddard Institute for Space Studies, New York, NY 10025, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Columbia University Earth Institute, New York, NY 10027, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Centre National de la Recherche Scientifique, LOCEAN Paris, hosted by Ifremer, Brest, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>12</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>24</issue>
<fpage>13421</fpage>
<lpage>13449</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/13421/2011/acp-11-13421-2011.html">This article is available from http://www.atmos-chem-phys.net/11/13421/2011/acp-11-13421-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/13421/2011/acp-11-13421-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/13421/2011/acp-11-13421-2011.pdf</self-uri>
<abstract>
<p>Improving observations of ocean heat content show that Earth
is absorbing more energy from the Sun than it is radiating to space as heat,
even during the recent solar minimum. The inferred planetary energy
imbalance, 0.58 Â± 0.15 W m&lt;sup&gt;âˆ’2&lt;/sup&gt; during the 6-yr period 2005â€“2010,
confirms the dominant role of the human-made greenhouse effect in driving
global climate change. Observed surface temperature change and ocean heat
gain together constrain the net climate forcing and ocean mixing rates. We
conclude that most climate models mix heat too efficiently into the deep
ocean and as a result underestimate the negative forcing by human-made
aerosols. Aerosol climate forcing today is inferred to be âˆ’1.6 Â± 0.3 W m&lt;sup&gt;âˆ’2&lt;/sup&gt;,
implying substantial aerosol indirect climate forcing via cloud
changes. Continued failure to quantify the specific origins of this large
forcing is untenable, as knowledge of changing aerosol effects is needed to
understand future climate change. We conclude that recent slowdown of ocean
heat uptake was caused by a delayed rebound effect from Mount Pinatubo
aerosols and a deep prolonged solar minimum. Observed sea level rise during
the Argo float era is readily accounted for by ice melt and ocean thermal
expansion, but the ascendency of ice melt leads us to anticipate
acceleration of the rate of sea level rise this decade.</p>
</abstract>
<counts><page-count count="29"/></counts>
</article-meta>
</front>
<body/>
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