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Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy...

Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_1bfa61e517b646b191629910b1307da1

Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach

About this item

Full title

Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach

Author / Creator

Publisher

Katlenburg-Lindau: Copernicus GmbH

Journal title

Climate of the past, 2017-07, Vol.13 (7), p.819-832

Language

English

Formats

Publication information

Publisher

Katlenburg-Lindau: Copernicus GmbH

More information

Scope and Contents

Contents

Glacial cycles of the late Quaternary are controlled by the asymmetrically varying mass balance of continental ice sheets in the Northern Hemisphere. Surface mass balance is governed by processes of ablation and accumulation. Here two ablation schemes, the positive-degree-day (PDD) method and the surface energy balance (SEB) approach, are compared...

Alternative Titles

Full title

Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_1bfa61e517b646b191629910b1307da1

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_1bfa61e517b646b191629910b1307da1

Other Identifiers

ISSN

1814-9332,1814-9324

E-ISSN

1814-9332

DOI

10.5194/cp-13-819-2017

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