<?xml version="1.0" encoding="UTF-8"?>

<?xml-stylesheet type="text/xsl" href="/static/oaitohtml.xsl"?>

<!--
<?xml-stylesheet type="text/xsl" href="/oaitohtml.xsl"?>
-->

<OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
    <responseDate>2026-10-13T08:03:47Z</responseDate>
    <request verb="GetRecord" metadataPrefix="oai_dc" identifier="10.57760/sciencedb.01829" >https://www.scidb.cn/oai</request>
<GetRecord>
    <record>
    <header >
    <identifier>10.57760/sciencedb.01829</identifier>
    <datestamp>2022-12-02T18:29:37Z</datestamp>
</header>
    <metadata>
        
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:date>2022-12-02</dc:date>
  <dc:title>A dataset of standard precipitation index reconstructed from multi-proxies over Asia for the past 300 years</dc:title>
  <dc:identifier>doi:10.57760/sciencedb.01829</dc:identifier>
  <dc:language>en</dc:language>
  <dc:description>Based on 2912 annually resolved proxy series mainly derived from tree-ring and historical documents (Metadata of Proxies.xlsx), we present a set of standard precipitation index (SPI) reconstructions for annual (Nov-Oct) covering entire Asia and for wet season (i.e., Nov-Apr for western Asia and May-Oct for the others) with the spatial resolution of 2.5&amp;deg; since 1700. The dataset of includes 4 SPI reconstructions: (1) the Nov-Oct SPI reconstruction for entire Asia without using tree-ring density chronologies and width chronologies with negative correlations to precipitation (Nov-Oct SPI Version A); (2) the Nov-Oct SPI reconstruction for entire Asia by adding tree-ring density chronologies and width chronologies with negative correlations to precipitation (Nov-Oct SPI Version B); (3) the wet season SPI reconstruction for the extra-tropical Asia (Nov-Apr SPI for western Asia and May-Oct SPI for the rest regions) without using tree-ring density chronologies and width chronologies with negative correlations to precipitation (wet season SPI Version A); (4) the wet season SPI reconstruction for the extra-tropical Asia (Nov-Apr SPI for western Asia and May-Oct SPI for the rest regions) by adding tree-ring density chronologies and width chronologies with negative correlations to precipitation (wet season SPI Version B). Each of them is stored in a NetCDF file (.nc) and contains 5 three-dimension (longitude &amp;times; latitude &amp;times; time) variables, including reconstructed SPI, adjusted coefficient of determination (R2a), validation RE, validation CE and the number of proxies used for construction (nPrx).</dc:description>
  <dc:subject>standard precipitation index; multi-proxies; climate reconstruction; Asia ; past 300 years</dc:subject>
  <dc:creator>Yang Liu</dc:creator>
  <dc:creator>Jingyun Zheng</dc:creator>
  <dc:creator>Zhixin Hao</dc:creator>
  <dc:creator>Quansheng Ge</dc:creator>
  <dc:rights>PUBLIC</dc:rights>
  <dc:rights>https://creativecommons.org/licenses/by/4.0/</dc:rights>
  <dc:type>dataset</dc:type>
  <dc:publisher>Science Data Bank</dc:publisher>
</oai_dc:dc>

    </metadata>
</record>
</GetRecord>
</OAI-PMH>