Reference:Reference-020617: Difference between revisions
From CSDMS
m Text replacement - " |CorpusID=" to " |CorpusID=" |
m Text replacement - "None" to "" |
||
| (One intermediate revision by one other user not shown) | |||
| Line 5: | Line 5: | ||
|Year=2023-11-09 | |Year=2023-11-09 | ||
|Journal=The Cryosphere | |Journal=The Cryosphere | ||
|Booktitle= | |Booktitle= | ||
|Volume=17 | |Volume=17 | ||
|Pages=4705–4727 | |Pages=4705–4727 | ||
| Line 16: | Line 16: | ||
|PublicationClusterID=0 | |PublicationClusterID=0 | ||
|MS_PublicationClusterID=0 | |MS_PublicationClusterID=0 | ||
|Semantic_ID=c2efe7af325c92b8a24d8d4afe6b4a1d9e44df5d | |Semantic_ID=c2efe7af325c92b8a24d8d4afe6b4a1d9e44df5d |CorpusID=259922065 | ||
|CorpusID=259922065 | |||
|PublicationWhatKindOf=a module application description | |PublicationWhatKindOf=a module application description | ||
|PublicationNrofModels=a single module | |PublicationNrofModels=a single module | ||
| Line 26: | Line 25: | ||
}} | }} | ||
{{RefsInt3 | {{RefsInt3 | ||
|PublicationAnimationsCargo= | |PublicationAnimationsCargo= | ||
}} | }} | ||
Latest revision as of 11:42, 12 November 2024
| Author(s) | McArthur, Koi; McCormack, Felicity S.; Dow, Christine F.; |
| BibType | journalArticle |
| Title | Basal conditions of Denman Glacier from glacier hydrology and ice dynamics modeling |
| Editors | |
| Year | 2023-11-09 |
| Journal | The Cryosphere |
| Booktitle | |
| Volume | 17 |
| Pages | 4705–4727 |
| URL | https://tc.copernicus.org/articles/17/4705/2023/ |
| DOI | 10.5194/tc-17-4705-2023 |
| ISBN | |
| Note | Auto downloaded ref at: 2024-08-16
|
| |
|
| Feature reference | No |
| PublicationClusterID | 0 |
| MS_PublicationClusterID | 0 |
| Semantic_ID | c2efe7af325c92b8a24d8d4afe6b4a1d9e44df5d |
| Nr of citations | 6 |
| 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: | ISSM
|
