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<titleInfo><title>The state of rock debris covering Earth’s glaciers</title></titleInfo>


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<name type="personal">
  <namePart type="given">Sam</namePart>
  <namePart type="family">Herreid</namePart>
  <role><roleTerm type="text">author</roleTerm> </role></name>
<name type="personal">
  <namePart type="given">Francesca</namePart>
  <namePart type="family">Pellicciotti</namePart>
  <role><roleTerm type="text">author</roleTerm> </role><identifier type="local">b28f055a-81ea-11ed-b70c-a9fe7f7b0e70</identifier></name>














<abstract lang="eng">Rock debris can accumulate on glacier surfaces and dramatically reduce glacier melt. The structure of a debris cover is unique to each glacier and sensitive to climate. Despite this, debris cover has been omitted from global glacier models and forecasts of their response to a changing climate. Fundamental to resolving these omissions is a global map of debris cover and an estimate of its future spatial evolution. Here we use Landsat imagery and a detailed correction to the Randolph Glacier Inventory to show that 7.3% of mountain glacier area is debris covered and over half of Earth’s debris is concentrated in three regions: Alaska (38.6% of total debris-covered area), Southwest Asia (12.6%) and Greenland (12.0%). We use a set of new metrics, which include stage, the current position of a glacier on its trajectory towards reaching its spatial carrying capacity of debris cover, to quantify the state of glaciers. Debris cover is present on 44% of Earth’s glaciers and prominent (&gt;1.0 km2) on 15%. Of Earth’s glaciers, 20% have a substantial percentage of debris cover for which the net stage is 36% and the bulk of individual glaciers have evolved beyond an optimal moraine configuration favourable for debris-cover expansion. Use of this dataset in global-scale models will enable improved estimates of melt over 10.6% of the global glacier domain.</abstract>

<originInfo><publisher>Springer Nature</publisher><dateIssued encoding="w3cdtf">2020</dateIssued>
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<language><languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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<subject><topic>General Earth and Planetary Sciences</topic>
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<relatedItem type="host"><titleInfo><title>Nature Geoscience</title></titleInfo>
  <identifier type="issn">1752-0894</identifier>
  <identifier type="eIssn">1752-0908</identifier><identifier type="doi">10.1038/s41561-020-0615-0</identifier>
<part><detail type="volume"><number>13</number></detail><detail type="issue"><number>9</number></detail><extent unit="pages">621-627</extent>
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     <url>https://doi.org/10.1038/s41561-020-0630-1</url>
  
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<mla>Herreid, Sam, and Francesca Pellicciotti. “The State of Rock Debris Covering Earth’s Glaciers.” &lt;i&gt;Nature Geoscience&lt;/i&gt;, vol. 13, no. 9, Springer Nature, 2020, pp. 621–27, doi:&lt;a href=&quot;https://doi.org/10.1038/s41561-020-0615-0&quot;&gt;10.1038/s41561-020-0615-0&lt;/a&gt;.</mla>
<short>S. Herreid, F. Pellicciotti, Nature Geoscience 13 (2020) 621–627.</short>
<ama>Herreid S, Pellicciotti F. The state of rock debris covering Earth’s glaciers. &lt;i&gt;Nature Geoscience&lt;/i&gt;. 2020;13(9):621-627. doi:&lt;a href=&quot;https://doi.org/10.1038/s41561-020-0615-0&quot;&gt;10.1038/s41561-020-0615-0&lt;/a&gt;</ama>
<ieee>S. Herreid and F. Pellicciotti, “The state of rock debris covering Earth’s glaciers,” &lt;i&gt;Nature Geoscience&lt;/i&gt;, vol. 13, no. 9. Springer Nature, pp. 621–627, 2020.</ieee>
<chicago>Herreid, Sam, and Francesca Pellicciotti. “The State of Rock Debris Covering Earth’s Glaciers.” &lt;i&gt;Nature Geoscience&lt;/i&gt;. Springer Nature, 2020. &lt;a href=&quot;https://doi.org/10.1038/s41561-020-0615-0&quot;&gt;https://doi.org/10.1038/s41561-020-0615-0&lt;/a&gt;.</chicago>
<apa>Herreid, S., &amp;#38; Pellicciotti, F. (2020). The state of rock debris covering Earth’s glaciers. &lt;i&gt;Nature Geoscience&lt;/i&gt;. Springer Nature. &lt;a href=&quot;https://doi.org/10.1038/s41561-020-0615-0&quot;&gt;https://doi.org/10.1038/s41561-020-0615-0&lt;/a&gt;</apa>
<ista>Herreid S, Pellicciotti F. 2020. The state of rock debris covering Earth’s glaciers. Nature Geoscience. 13(9), 621–627.</ista>
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