Reference:Reference-001123: Difference between revisions
From CSDMS
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{{ | {{BibEntryCargo | ||
| | |Firstname=Greve, Ralf; Wyrwoll, Karl-Heinz; Eisenhauer, Anton; | ||
|BibType=journalArticle | |||
|Title=Deglaciation of the Northern Hemisphere at the onset of the Eemian and Holocene | |||
|Year=1999-01-01 | |||
|Journal=Annals of Glaciology | |||
|Booktitle= | |||
|Volume=28 | |||
|Pages=1–8 | |||
|URL=https://www.cambridge.org/core/product/identifier/S0260305500265440/type/journal_article | |||
|DOI=10.3189/172756499781821643 | |||
|Note=Auto downloaded ref at: 2019-12-31 | |||
}} | }} | ||
{{RefsInt1 | {{RefsInt1 | ||
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|MS_PublicationClusterID=1983641981 | |MS_PublicationClusterID=1983641981 | ||
|PublicationWhatKindOf=a module application description | |PublicationWhatKindOf=a module application description | ||
|PublicationNrofModels=a single module | |||
|PublicationHPCCYesno=No | |PublicationHPCCYesno=No | ||
}} | }} | ||
{{RefsInt2 | {{RefsInt2 | ||
|PublicationMultipleModelsCargo=SICOPOLIS | |PublicationMultipleModelsCargo=SICOPOLIS | ||
}} | }} | ||
Revision as of 21:58, 31 December 2019
| Author(s) | Greve, Ralf; Wyrwoll, Karl-Heinz; Eisenhauer, Anton; |
| BibType | journalArticle |
| Title | Deglaciation of the Northern Hemisphere at the onset of the Eemian and Holocene |
| Editors | |
| Year | 1999-01-01 |
| Journal | Annals of Glaciology |
| Booktitle | |
| Volume | 28 |
| Pages | 1–8 |
| URL | https://www.cambridge.org/core/product/identifier/S0260305500265440/type/journal_article |
| DOI | 10.3189/172756499781821643 |
| ISBN | |
| Note | Auto downloaded ref at: 2019-12-31
|
| |
|
| Feature reference | No |
| PublicationClusterID | 0 |
| MS_PublicationClusterID | 1983641981 |
| Semantic_ID | {{{Semantic_ID}}} |
| Nr of citations | Template:SEM |
| Sort of publication | a module application description |
| Sort of model publication | a single module |
| Is the CSDMS HPC used | No |
| If HPC is used, for what project was it?: | |
| Associated simulation movie if any: |
|
| Model(s) discussed: | SICOPOLIS |
