Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales
Factors driving ice flow variability in Greenland vary by timescale. At seasonal scale, Helheim Glacier ice velocity responds most strongly to meltwater runoff. Glacier terminus position drives velocity variability at longer time scales.
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2022-10-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-022-33292-y |
| _version_ | 1798029801077866496 |
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| author | Lizz Ultee Denis Felikson Brent Minchew Leigh A. Stearns Bryan Riel |
| author_facet | Lizz Ultee Denis Felikson Brent Minchew Leigh A. Stearns Bryan Riel |
| author_sort | Lizz Ultee |
| collection | DOAJ |
| description | Factors driving ice flow variability in Greenland vary by timescale. At seasonal scale, Helheim Glacier ice velocity responds most strongly to meltwater runoff. Glacier terminus position drives velocity variability at longer time scales. |
| first_indexed | 2024-04-11T19:31:13Z |
| format | Article |
| id | doaj.art-cce91817534b435b90e5e8d6b0619d31 |
| institution | Directory Open Access Journal |
| issn | 2041-1723 |
| language | English |
| last_indexed | 2024-04-11T19:31:13Z |
| publishDate | 2022-10-01 |
| publisher | Nature Portfolio |
| record_format | Article |
| series | Nature Communications |
| spelling | doaj.art-cce91817534b435b90e5e8d6b0619d312022-12-22T04:07:00ZengNature PortfolioNature Communications2041-17232022-10-0113111010.1038/s41467-022-33292-yHelheim Glacier ice velocity variability responds to runoff and terminus position change at different timescalesLizz Ultee0Denis Felikson1Brent Minchew2Leigh A. Stearns3Bryan Riel4Dept. of Earth & Climate Sciences, Middlebury CollegeCryospheric Sciences Laboratory, NASA Goddard Space Flight CenterDept. of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of TechnologyDepartment of Geology, University of KansasDept. of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of TechnologyFactors driving ice flow variability in Greenland vary by timescale. At seasonal scale, Helheim Glacier ice velocity responds most strongly to meltwater runoff. Glacier terminus position drives velocity variability at longer time scales.https://doi.org/10.1038/s41467-022-33292-y |
| spellingShingle | Lizz Ultee Denis Felikson Brent Minchew Leigh A. Stearns Bryan Riel Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales Nature Communications |
| title | Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales |
| title_full | Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales |
| title_fullStr | Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales |
| title_full_unstemmed | Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales |
| title_short | Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales |
| title_sort | helheim glacier ice velocity variability responds to runoff and terminus position change at different timescales |
| url | https://doi.org/10.1038/s41467-022-33292-y |
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