dc.contributor.author | Dahl-Jensen, Dorthe | |
dc.contributor.author | Gundestrup, N. S. | |
dc.contributor.author | Keller, K. | |
dc.contributor.author | Johnsen, S. J. | |
dc.contributor.author | Gogineni, Sivaprasad | |
dc.contributor.author | Allen, Christopher Thomas | |
dc.contributor.author | Chuah, T. S. | |
dc.contributor.author | Miller, H. | |
dc.contributor.author | Kipfstuhl, S. | |
dc.contributor.author | Waddington, E. D. | |
dc.date.accessioned | 2015-12-17T22:28:25Z | |
dc.date.available | 2015-12-17T22:28:25Z | |
dc.date.issued | 1997 | |
dc.identifier.citation | Dahl-Jensen, D., N. S. Gundestrup, K. Keller, S. J. Johnsen, S. P. Gogineni, C. T. Allen, T. S. Chuah, H. Miller, S. Kipfstuhl, and E. D. Waddington. "A Search in North Greenland for a New Ice-core Drill Site." Journal of Glaciology 43.144 (1997): 300-06. | en_US |
dc.identifier.uri | http://hdl.handle.net/1808/19277 | |
dc.description | This is the published version. Copyright International Glaciological Society | en_US |
dc.description.abstract | A new deep ice-core drilling site has been identified in north Greenland at 75.12 ° N, 42 .30 ° W, 316 km north-northwest (NNW) of the GRIP drill site on the summit of the ice sheet. The ice thickness here is 3085 m; the surface elevation is 2919 m. The North GRIP (NG RIP) site is identified so that ice of Eemian age (115- 130 ka BP, calendar years before present ) is located as far above bedrock as possible and so the thickness of the Eemian layer is as great as possible. An ice-flow model, similar to the one used to date the GRIP ice core, is used to simulate the flow along the NNW-trending ice ridge. Surface and bedrock elevations, surface accumulation-rate distribution and radio-echo sounding along the ridge have been used as model input. The surface accumulation rate drops from 0.23 mice equivalent year 1 at GRIP to 0.19 mice equivalent year- 1 50 km from GRIP. Over the following 300 km the accumulation is relatively constant, before it starts decreasing again further north. Ice thicknesses up to 3250 m bring the temperature of the basal ice up to the pressure-melting point 100- 250 km from GRIP. The NGRIP site is located 316 km from GRIP in a region where the bedrock is smooth and the accumulation rate is 0.19 m ice equivalent year 1 • The modeled basal ice here has always been a few degrees below the pressure-melting point. Internal radio-echo sounding horizons can be traceq between the GRIP and NGRIP sites, allowing us to date the ice down to 2300 m depth (52 ka BP ). An ice-flow model predicts that the Eemian-age ice will be located in the depth range 2710 - 2800 m, which is 285 m above the bedrock. This is 120 m further above the bedrock, and the thickness of the Eemian layer of ice is 20 m thicker, than at the GRIP ice-core ite. | en_US |
dc.publisher | International Glaciological Society | en_US |
dc.relation.isversionof | http://www.igsoc.org/journal/ | en_US |
dc.title | A search in north Greenland for a new ice-core drill site | en_US |
dc.type | Article | |
kusw.kuauthor | Allen, Christopher Thomas | |
kusw.kudepartment | Electrical Engr & Comp Science | en_US |
dc.identifier.orcid | https://orcid.org/0000-0002-1474-1948 | |
kusw.oaversion | Scholarly/refereed, publisher version | |
kusw.oapolicy | This item does not meet KU Open Access policy criteria. | |
dc.rights.accessrights | openAccess | |