Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier.

about

Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier.

Item

http://www.wikidata.org/entity/Q42670342

description

2017 nî lūn-bûn

@nan

2017年の論文

@ja

2017年論文

@yue

2017年論文

@zh-hant

2017年論文

@zh-hk

2017年論文

@zh-mo

2017年論文

@zh-tw

2017年论文

@wuu

2017年论文

@zh

2017年论文

@zh-cn

name

Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier.

@en

Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier.

@nl

type

Item

label

Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier.

@en

Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier.

@nl

prefLabel

Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier.

@en

Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier.

@nl

P1476

Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier.

@en

P2093

Fanny Kaczmar

http://www.w3.org/2001/XMLSchema#string

Laurence M Dyke

http://www.w3.org/2001/XMLSchema#string

Mads Faurschou Knudsen

http://www.w3.org/2001/XMLSchema#string

Marie-Alexandrine Sicre

http://www.w3.org/2001/XMLSchema#string

Martin W Miles

http://www.w3.org/2001/XMLSchema#string

Ulla Kokfelt

http://www.w3.org/2001/XMLSchema#string

Vincent Klein

http://www.w3.org/2001/XMLSchema#string

P2860

Changes in the velocity structure of the Greenland Ice Sheet

Abrupt Holocene climate change as an important factor for human migration in West Greenland

Acceleration of Jakobshavn Isbræ triggered by warm subsurface ocean waters

Solar forcing of regional climate change during the Maunder Minimum.

Spatial and temporal distribution of mass loss from the Greenland Ice Sheet since AD 1900.

Influence of the Atlantic subpolar gyre on the thermohaline circulation.

North Atlantic warming and the retreat of Greenland's outlet glaciers.

Persistent positive North Atlantic oscillation mode dominated the Medieval Climate Anomaly.

Past temperatures directly from the greenland ice sheet

The early medieval warm epoch and its sequel

P2888

s41598-017-13246-x

P304

13626

http://www.w3.org/2001/XMLSchema#string

P31

scholarly article

P356

10.1038/S41598-017-13246-X

http://www.w3.org/2001/XMLSchema#string

P407

English

P433

http://www.w3.org/2001/XMLSchema#string

P478

http://www.w3.org/2001/XMLSchema#string

P50

David Wangner

Camilla S Andresen

P577

2017-10-19T00:00:00Z

http://www.w3.org/2001/XMLSchema#dateTime

P6179

1092212923

http://www.w3.org/2001/XMLSchema#string

P698

29051588

http://www.w3.org/2001/XMLSchema#string

P921

Greenland

Akullnaja

P932

5648833

http://www.w3.org/2001/XMLSchema#string