Thermokarst rates intensify due to climate change and forest fragmentation in an Alaskan boreal forest lowland. - Wikidata - awgldk - TriplyDB

Thermokarst rates intensify due to climate change and forest fragmentation in an Alaskan boreal forest lowland.

Thermokarst rates intensify due to climate change and forest fragmentation in an Alaskan boreal forest lowland.

http://www.wikidata.org/entity/Q31004779

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Regional atmospheric cooling and wetting effect of permafrost thaw-induced boreal forest loss.Threshold loss of discontinuous permafrost and landscape evolution.The positive net radiative greenhouse gas forcing of increasing methane emissions from a thawing boreal forest-wetland landscape.Direct and indirect climate change effects on carbon dioxide fluxes in a thawing boreal forest-wetland landscape.The role of driving factors in historical and projected carbon dynamics of upland ecosystems in Alaska.In situ nuclear magnetic resonance response of permafrost and active layer soil in boreal and tundra ecosystems Remote Sensing of Landscape Change in Permafrost Regions Influence of Holocene permafrost aggradation and thaw on the paleoecology and carbon storage of a peatland complex in northwestern Canada

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Thermokarst rates intensify due to climate change and forest fragmentation in an Alaskan boreal forest lowland.

http://www.wikidata.org/entity/Q31004779

description

2015 nî lūn-bûn

@nan

2015 թուականի Հոկտեմբերին հրատարակուած գիտական յօդուած

@hyw

2015 թվականի հոտեմբերին հրատարակված գիտական հոդված

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2015年の論文

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2015年論文

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2015年論文

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2015年論文

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2015年論文

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2015年論文

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2015年论文

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Thermokarst rates intensify du ...... Alaskan boreal forest lowland.

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Thermokarst rates intensify du ...... Alaskan boreal forest lowland.

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Global Change Biology

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Thermokarst rates intensify du ...... Alaskan boreal forest lowland.

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Amy Breen

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Anthony D McGuire

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Dana R N Brown

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Eugénie S Euskirchen

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Hélène Genet

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Mark J Lara

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Mark T Jorgenson

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William R Bolton

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Yujin Zhang

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P2860

Permafrost Thaw Accelerates in Boreal Peatlands During Late-20th Century Climate Warming

Disequilibrium response of permafrost in boreal continental western Canada to climate change

Observations of Thermokarst and Its Impact on Boreal Forests in Alaska, U.S.A

The resilience and functional role of moss in boreal and arctic ecosystems.

Polygonal tundra geomorphological change in response to warming alters future CO2 and CH4 flux on the Barrow Peninsula.

Climate change and the permafrost carbon feedback.

Changes in the structure and function of northern Alaskan ecosystems when considering variable leaf-out times across groupings of species in a dynamic vegetation model.

Forests on thawing permafrost: fragmentation, edge effects, and net forest loss.

A working guide to boosted regression trees.

Boosted trees for ecological modeling and prediction.

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scholarly article

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10.1111/GCB.13124

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2

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22

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Vladimir E. Romanovsky

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2015-10-13T00:00:00Z

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282872767

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26463267

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