<?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>2026-10-11T16:03:24Z</responseDate>
    <request verb="GetRecord" metadataPrefix="oai_dc" identifier="10.57760/sciencedb.43590" >https://www.scidb.cn/oai</request>
<GetRecord>
    <record>
    <header >
    <identifier>10.57760/sciencedb.43590</identifier>
    <datestamp>2026-08-28T10:44:23Z</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>2026-08-28</dc:date>
  <dc:title>Neglecting diel dynamics underestimates Global lakes CO2 emissions by almost 20%</dc:title>
  <dc:identifier>doi:10.57760/sciencedb.43590</dc:identifier>
  <dc:language>en</dc:language>
  <dc:description>Global lake CO2 emission estimates rely heavily on temporally sparse observations, yet the extent to which daytime sampling biases whole-day fluxes remains unresolved. Here we synthesize 616 high-frequency diel CO2 flux observations from 158 lakes worldwide to quantify this bias and identify its environmental controls. Nighttime fluxes were, on average, 27% higher than daytime fluxes, with 69% of lakes exhibiting a night-enhanced regime (NER) driven mainly by productive, shallow and low-latitude systems. Notably, 22% of lakes shifted from daytime CO2 uptake to nighttime emission, indicating potential misclassification of lake source-sink status. A contrasting day-enhanced regime (DER) occurred more frequently in dissolved organic carbon (DOC)-rich and higher-latitude lakes. The strength of diel asymmetry increased with chlorophyll-a (Chl-a) under low-to-moderate productivity but saturated under high trophic conditions. Incorporating diel variability increased global lake CO2 emissions from 357 to 439 Tg C yr&amp;minus;1, exposing a significant underestimation of 20% (82 Tg C yr&amp;minus;1). These findings reveal a previously under-resolved temporal bias in global lake carbon budgets and provide a regime-specific diel correction framework for improving lake CO2 emission estimates.</dc:description>
  <dc:subject>lake; CO2; diel</dc:subject>
  <dc:creator>Lejun Zhao</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>