Meteorological observations 1998 at the arctic station, Qeqertarsuaq (69°15'N), Central West Greenland/Active layer monitoring in two Greenlandic permafrost areas
Zackenberg and Disko Island
Datos Bibliográficos
| ID | 9849448 |
|---|---|
| Autores | Ole Humlum (University of Copenhagen, autor de correspondencia), Birger Ulf Hansen (0000-0002-5440-6925, University of Copenhagen), Niels Nielsen (University of Copenhagen), Hanne H Christiansen (0000-0002-6218-3493, University of Copenhagen) |
| Año | 1999 |
| Volumen | 99 |
| Número | 1 |
| Páginas | 113-121 |
| Fecha de publicación | 1999-01-01 |
| Peer Reviewed | Sí |
| Open Access | No |
| Tipo | ARTICLE |
| Revista | Geografisk Tidsskrift-Danish Journal of Geography (JOURNAL) |
| Identificadores de la revista | ISSN: 0016-7223 • E-ISSN: 1903-2471 |
| Editorial | Informa UK Limited (PUBLISHER • GB) |
| DOI | 10.1080/00167223.1999.10649428 |
| OpenAlex | W2321859800 |
| Idioma | EN |
| Citas recibidas | 4 |
| Referencias citadas | 9 |
An automatic meteorological station has been operating at the Arctic Station (69°15'N, 53°31'W) in West Greenland since 1990. This paper summarises meteorological parameters during 1998, including snow cover, ground temperatures and active layer development, and presents comments on the local permafrost thickness. Abstract Active layer monitoring in Greenland was started in 1996 and 1997, and forms part of the Circumpolar Active Layer Monitoring (CALM) Network of the International Permafrost Association (IPA). The results of the first years of this monitoring of thaw progression and maximum active layer thickness in two Greenlandic permafrost areas are presented. Two sites are in the continuous permafrost zone at Zackenberg in NE Greenland (74 °N), and one at Disko Island in W Greenland (69 °N), at the border between discontinuous and continuous permafrost. The data collected at Zackenberg demonstrate interannual variation in the timing of thaw progression in the monitoring grid holding a seasonal snowpatch, while there is less variation in the horizontal grid without a snowpatch. The maximum active layer thickness for the two Zackenberg grids is more or less consistent for the first three years with averages from 58 to 66 cm in mid and late August. At Disko the active layer reached 71 cm in mid August 1998. Spatially the distribution of the maximum, annual active layer thickness within the grids is concordant
Active layer · Arctic · Atmospheric sciences · Circumpolar star · Climatology · Elevation (ballistics · Geography · Geomorphology · Layer (electronics · Permafrost · Physical geography · Snow · Snow cover · Arctic and Antarctic ice dynamics · Climate change and permafrost · Cryospheric studies and observations · Environmental Science · Geology · Oceanography
The circumpolar active layer monitoring (calm) program
Role of landscape parameters in riverine run-off, and sediment and organic matter yield on Disko Island, West Greenland
Meteorological Observations in 2000 at the Arctic Station, Qeqertarsuaq (69°15'N), Central West Greenland
Meteorological observations 1998 at the arctic station, Qeqertarsuaq (69°15'N), Central West Greenland/Active layer monitoring in two Greenlandic permafrost areas
| Obras citantes distintas | 4 |
|---|---|
| Citas por año | 0,15 |
| Intervalo de citas | 1999 - 2003 (5) |
| Velocidad de citación | historical |
| Altamente citado | No |
| Tipos de cita | Neutras: 4 |