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Record #187854:

Hydrology and transport of sediment and solutes at Zackenberg / Bent Hasholt.

Title: Hydrology and transport of sediment and solutes at Zackenberg / Bent Hasholt.
Author(s): Hasholt, Bent.
Date: 2008.
Publisher: Amsterdam: Academic Press
In: High-Arctic ecosystem dynamics in a changing climate : ten years of monitoring and research at Zackenberg Research Station, northeast Greenland. (2008.),
Abstract: Discusses hydrology and sediment and solute transport in Zackenberg area in relation to climate variability between 1995-2005. Results indicate decreasing precipitation and increasing evaporotranspiration during study years. Theoretically, this should result in decreasing run-off, but no such trend can be identified.
Notes:

In: High-Arctic ecosystem dynamics in a changing climate : ten years of monitoring and research at Zackenberg Research Station, northeast Greenland / Hans Meltofte, and 4 others, eds.

Keywords: 551.578 -- Precipitation, particular forms.
551.578.46 -- Snow cover and snow patches.
551.579 -- Hydrometeorology.
551.579.2 -- Water supply from snow.
556 -- Hydrology.
556.51 -- River basins and watersheds.
556.555.6 -- Lakes, sediments.
C -- Oceanography, hydrography and hydrology.
(*3) -- Arctic regions.
(*38) -- Greenland.
(*387) -- North Greenland.
SPRI record no.: 187854

MARCXML

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001 SPRI-187854
005 20221003135601.0
007 ta
008 221003s2008####ne#a###|#####|0||#0#eng#d
035 ## ‡aSPRI-187854
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aHasholt, Bent.
245 10 ‡aHydrology and transport of sediment and solutes at Zackenberg /‡cBent Hasholt.
260 ## ‡aAmsterdam :‡bAcademic Press,‡c2008.
300 ## ‡ap. 196-221 :‡bill., diags.
500 ## ‡aIn: High-Arctic ecosystem dynamics in a changing climate : ten years of monitoring and research at Zackenberg Research Station, northeast Greenland / Hans Meltofte, and 4 others, eds.
520 3# ‡aDiscusses hydrology and sediment and solute transport in Zackenberg area in relation to climate variability between 1995-2005. Results indicate decreasing precipitation and increasing evaporotranspiration during study years. Theoretically, this should result in decreasing run-off, but no such trend can be identified.
530 ## ‡aAlso issued online ‡uurn:doi:10.1016/S0065-2504(07)00009-8‡uhttps://dx.doi.org/10.1016/S0065-2504(07)00009-8
650 07 ‡a551.578 -- Precipitation, particular forms.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a551.579 -- Hydrometeorology.‡2udc
650 07 ‡a551.579.2 -- Water supply from snow.‡2udc
650 07 ‡a556 -- Hydrology.‡2udc
650 07 ‡a556.51 -- River basins and watersheds.‡2udc
650 07 ‡a556.555.6 -- Lakes, sediments.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
651 #7 ‡a(*387) -- North Greenland.‡2udc
773 0# ‡7nnam ‡aHans Meltofte, and 4 others, eds. ‡tHigh-Arctic ecosystem dynamics in a changing climate : ten years of monitoring and research at Zackenberg Research Station, northeast Greenland. ‡dAmsterdam : Academic Press, 2008. ‡wSPRI-185808
916 ## ‡a2009/08/11 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221003 ‡bJW