<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "https://jats.nlm.nih.gov/nlm-dtd/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" specific-use="SMUR" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">CPD</journal-id>
<journal-title-group>
<journal-title>Climate of the Past Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">CPD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Clim. Past Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1814-9359</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/cp-2021-2</article-id>
<title-group>
<article-title>Overcoming model instability in tree-ring-based temperature 
reconstructions using a multi-species method: A case study from the 
Changbai Mountains, northeastern China</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhu</surname>
<given-names>Liangjun</given-names>
<ext-link>https://orcid.org/0000-0003-0111-1450</ext-link>
</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>Liu</surname>
<given-names>Shuguang</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhu</surname>
<given-names>Haifeng</given-names>
<ext-link>https://orcid.org/0000-0001-9968-7284</ext-link>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cooper</surname>
<given-names>David J.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yuan</surname>
<given-names>Danyang</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhu</surname>
<given-names>Yu</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Li</surname>
<given-names>Zongshan</given-names>
<ext-link>https://orcid.org/0000-0003-0826-7271</ext-link>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhang</surname>
<given-names>Yuandong</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Liang</surname>
<given-names>Hanxue</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhang</surname>
<given-names>Xu</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Song</surname>
<given-names>Wenqi</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wang</surname>
<given-names>Xiaochun</given-names>
<ext-link>https://orcid.org/0000-0002-8897-5077</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>National Engineering Laboratory for Applied Technology of Forestry &amp; Ecology in South China, College of Life Science and Technology,  Central South University of Forestry and Technology, Changsha 410004, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Center for Ecological Research and Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of  Forestry, Northeast Forestry University, Harbin 150040, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100864, China</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Forest and Rangeland Stewardship, Colorado State University, Fort Collins, CO 80523, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences,  Beijing 100085, China</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Key Laboratory of Forest Ecology and Environment of National Forestry and Grassland Administration, Research Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Institute of Loess Plateau, Shanxi University, Taiyuan 030006, China</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>College of Forestry, Northwest A&amp;F University, Yangling 712100, China</addr-line>
</aff>
<funding-group>
<award-group id="gs1">
<funding-source>Hunan Provincial Science and Technology Department</funding-source>
<award-id>2020RC2058</award-id>
</award-group>
<award-group id="gs2">
<funding-source>China Postdoctoral Science Foundation</funding-source>
<award-id>2020M682600</award-id>
</award-group>
<award-group id="gs3">
<funding-source>Education Department of Hunan Province</funding-source>
<award-id>20B627</award-id>
</award-group>
<award-group id="gs4">
<funding-source>Central South University of Forestry and Technology</funding-source>
<award-id>2020YJ012</award-id>
</award-group>
</funding-group>
<pub-date pub-type="epub">
<day>11</day>
<month>01</month>
<year>2021</year>
</pub-date>
<volume>2021</volume>
<fpage>1</fpage>
<lpage>19</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2021 Liangjun Zhu et al.</copyright-statement>
<copyright-year>2021</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://cp.copernicus.org/preprints/cp-2021-2/">This article is available from https://cp.copernicus.org/preprints/cp-2021-2/</self-uri>
<self-uri xlink:href="https://cp.copernicus.org/preprints/cp-2021-2/cp-2021-2.pdf">The full text article is available as a PDF file from https://cp.copernicus.org/preprints/cp-2021-2/cp-2021-2.pdf</self-uri>
<abstract>
<p>&lt;p&gt;The unstable sensitivity of growth-climate relationships greatly restricts tree-ring-based paleoclimate reconstructions, especially in areas with frequent &lt;q&gt;divergence&lt;/q&gt; problems, such as the temperate zone in northeast China. Here, we propose an original tree-species mixing method to overcome this obstacle and improve the stability and reliability of reconstruction models. We take the tree-ring based growing-season minimum temperature reconstruction for the northern Changbai Mountains in northeast China as an example to illustrate the method. Compared with previous temperature reconstruction models, our reconstruction model is more stable and reliable and explains up to 68&amp;thinsp;% of the variance. It is also highly consistent with historical records and tree-ring-based temperature reconstructions from the nearby Xiaoxing&apos;an Mountains and from across the Northern Hemisphere. Our reconstruction uses two different tree species and is more accurate than temperature reconstructions developed from a single species. Over the past 259 years (AD 1757&amp;ndash;2015), five significant cold periods and five warm periods were identified. The reconstruction indicates rapid warming since the 1980s, which is consistent with other instrumental and reconstructed records. We also found the Atlantic Multidecadal Oscillation plays a crucial role in driving the growing-season minimum temperature in the northern Changbai Mountains.&lt;/p&gt;</p>
</abstract>
<counts><page-count count="19"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>