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<front>
<journal-meta>
<journal-id journal-id-type="publisher">CP</journal-id>
<journal-title-group>
<journal-title>Climate of the Past</journal-title>
<abbrev-journal-title abbrev-type="publisher">CP</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Clim. Past</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1814-9332</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/cp-8-227-2012</article-id>
<title-group>
<article-title>Northern Hemisphere temperature patterns in the last 12 centuries</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ljungqvist</surname>
<given-names>F. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Krusic</surname>
<given-names>P. J.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Brattström</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sundqvist</surname>
<given-names>H. S.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of History, Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Centre for Medieval Studies, Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Bert Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Physical Geography and Quaternary Geology, Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Mathematics, Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<pub-date pub-type="epub">
<day>03</day>
<month>02</month>
<year>2012</year>
</pub-date>
<volume>8</volume>
<issue>1</issue>
<fpage>227</fpage>
<lpage>249</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 F. C. Ljungqvist et al.</copyright-statement>
<copyright-year>2012</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://cp.copernicus.org/articles/8/227/2012/cp-8-227-2012.html">This article is available from https://cp.copernicus.org/articles/8/227/2012/cp-8-227-2012.html</self-uri>
<self-uri xlink:href="https://cp.copernicus.org/articles/8/227/2012/cp-8-227-2012.pdf">The full text article is available as a PDF file from https://cp.copernicus.org/articles/8/227/2012/cp-8-227-2012.pdf</self-uri>
<abstract>
<p>We analyse the spatio-temporal patterns of temperature variability over
Northern Hemisphere land areas, on centennial time-scales, for the last 12
centuries using an unprecedentedly large network of temperature-sensitive
proxy records. Geographically widespread positive temperature anomalies are
observed from the 9th to 11th centuries, similar in extent and magnitude to
the 20th century mean. A dominance of widespread negative anomalies is
observed from the 16th to 18th centuries. Though we find the amplitude and
spatial extent of the 20th century warming is within the range of
natural variability over the last 12 centuries, we also find that the rate
of warming from the 19th to the 20th century is unprecedented in
the context of the last 1200 yr. The positive Northern Hemisphere
temperature change from the 19th to the 20th century is clearly the largest
between any two consecutive centuries in the past 12 centuries. These
results remain robust even after removing a significant number of proxies in
various tests of robustness showing that the choice of proxies has no
particular influence on the overall conclusions of this study.</p>
</abstract>
<counts><page-count count="23"/></counts>
</article-meta>
</front>
<body/>
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