Zobrazeno 1 - 10
of 23
pro vyhledávání: '"OLE B. OLESEN"'
Autor:
HORST MACHGUTH, HENRIK H. THOMSEN, ANKER WEIDICK, ANDREAS P. AHLSTRØM, JAKOB ABERMANN, MORTEN L. ANDERSEN, SIGNE B. ANDERSEN, ANDERS A. BJØRK, JASON E. BOX, ROGER J. BRAITHWAITE, CARL E. BØGGILD, MICHELE CITTERIO, POUL CLEMENT, WILLIAM COLGAN, ROBERT S. FAUSTO, KARIN GLEIE, STEFANIE GUBLER, BENT HASHOLT, BERNHARD HYNEK, NIELS T. KNUDSEN, SIGNE H. LARSEN, SEBASTIAN H. MERNILD, JOHANNES OERLEMANS, HANS OERTER, OLE B. OLESEN, C. J. P. PAUL SMEETS, KONRAD STEFFEN, MANFRED STOBER, SHIN SUGIYAMA, DIRK VAN AS, MICHIEL R. VAN DEN BROEKE, RODERIK S. W. VAN DE WAL
Publikováno v:
Journal of Glaciology, Vol 62, Pp 861-887 (2016)
Glacier surface mass-balance measurements on Greenland started more than a century ago, but no compilation exists of the observations from the ablation area of the ice sheet and local glaciers. Such data could be used in the evaluation of modelled su
Externí odkaz:
https://doaj.org/article/d2e6bb1236a447a8b769b2696e8a5eed
Autor:
Ole B. Olesen1 ole@sam.sdu.dk, N. C. Petersen1 ncp@sam.sdu.dk
Publikováno v:
Journal of Productivity Analysis. Nov2003, Vol. 20 Issue 3, p323-360. 38p. 3 Charts, 5 Graphs.
Autor:
Ole B. Olesen1 ole@sam.sdu.dk, N. C. Petersen1 ncp@sam.sdu.dk
Publikováno v:
Journal of Productivity Analysis. Nov2003, Vol. 20 Issue 3, p237-241. 5p.
Publikováno v:
Annals of Glaciology. 37:83-89
In theoretical treatments of tidal bending of floating glaciers, the glacier is usually modelled as an elastic beam with uniform thickness, resting on an elastic foundation. With a few exceptions, values of the elastic (Young’s) modulus E of ice de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::89b8958c595319c1fe7d9ade48a2732c
https://doi.org/10.3189/172756403781815663
https://doi.org/10.3189/172756403781815663
Autor:
Ole B. Olesen, Andreas P. Ahlstrøm, Christoph Mayer, Carl Egede Bøggild, Steffen Podlech, William B. Krabill
Publikováno v:
GEUS Bulletin. :150-156
NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Mayer, C., Bøggild, C. E., Podlech, S., Olesen, O. B., Ahlstrøm, A. P., & Krabill, W. (2002). Glaciolog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7335322291eeaf9a87f1746a1c639481
https://doi.org/10.34194/ggub.v191.5144
https://doi.org/10.34194/ggub.v191.5144
Autor:
Andreas P. Ahlstrøm, Ole B. Olesen, E. Lintz Christensen, K. Keller, Johan Jacob Mohr, Niels Reeh, C. Egede Bøggild
Publikováno v:
Annals of Glaciology. 34:309-314
The hydrological ice-sheet basin draining into the Tasersiaq lake, West Greenland (66°13’ N, 50°30’W), was delineated, first using standard digital elevation models (DEMs) for ice-sheet surface and bedrock, and subsequently using a new high-res
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0b1b98d995fff6ae9cd63ea80a4f794a
https://doi.org/10.3189/172756402781817860
https://doi.org/10.3189/172756402781817860
Publikováno v:
Annals of Glaciology. 31:111-117
Nioghalvfjerdsfjorden glacier is a >60 km long and 20 km wide floating outlet glacier located at 79°30’ N, 22° W, draining a large area of the northeast Greenland ice sheet. Climate, mass-balance and dynamics studies were carried out on the glaci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ecaf605c53483e5192bcf60b21a3a8b
https://doi.org/10.3189/172756400781820408
https://doi.org/10.3189/172756400781820408
Publikováno v:
Journal of Glaciology. 44:583-588
Ablation climate studies were made at two locations in northern Greenland in the summers of 1993 and 1994, respectively. Daily ablation was measured at ten stakes within a small area, and the data were compared with each other to detect gross errors.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b9f30ba1fe085706bf7e347ba7ce8684
https://doi.org/10.3189/s0022143000002094
https://doi.org/10.3189/s0022143000002094
Publikováno v:
Journal of Glaciology. 44:239-247
Reconnaissance energy-balance studies were made for the first time at two sites in North Greenland to compare with conditions in West Greenland. The field experiments were planned to save weight because it is expensive to operate in North Greenland.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::294c44cb04c5129fa59346bcf526c6b5
https://doi.org/10.1017/s0022143000002586
https://doi.org/10.1017/s0022143000002586
Publikováno v:
Science. 278:205-209
The report “North and northeast Greenland ice discharge from satellite radar interferometry” by E. J. Rignot et al . ([9 May, p. 934][1]) concludes that north and northeast Greenland glaciers are now discharging an excess of 8 cubic kilometers pe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44e614303f6e635963699dcb32e2f5ef
https://doi.org/10.1126/science.278.5336.205b
https://doi.org/10.1126/science.278.5336.205b