3 edition of Hydrological basins in West Greenland found in the catalog.
Hydrological basins in West Greenland
|Statement||by A. Weidick and O.B. Olesen.|
|Series||Rapport / Grønlands geologiske undersøgelse,, nr. 94, Rapport (Grønlands geologiske undersøgelse) ;, nr. 94.|
|Contributions||Olesen, O. B. 1937-|
|LC Classifications||QE70 .D43 nr. 94, GB835 .D43 nr. 94|
|The Physical Object|
|Pagination||51 p. :|
|Number of Pages||51|
|LC Control Number||81116467|
Read Volume 44 Issue 1 of Hydrology Research. Estimating daily reference evapotranspiration using available and estimated climatic data by adaptive neuro-fuzzy inference system (ANFIS) and artificial neural network (ANN). A new regional high-resolution map of basal and surface topography for the Greenland ice-sheet margin at Paakitsoq, West Greenland Ruth MOTTRAM,1 Claus NIELSEN,1 Andreas P. AHLSTRØM,1 Niels REEH,1,2 Steen S. KRISTENSEN,2 Erik L. CHRISTENSEN,2 Rene´ FORSBERG,2 Lars STENSENG2 1Geological Survey of Denmark and Greenland, Øster .
4 Antarctic Glaciology in the International Hydrological Decade. 5 Combined Heat, Ice and Water Balances at Selected Glacier Basins. A Guide for Compilation and Assemblage of Data for Glacier Mass Balance Measurements. 6 Textbooks on Hydrology. Analyses and Synoptic Tables of Contents of Selected Textbooks. Physical and chemical profiles of a shallow (c. m-deep) subsaline (total dissolved solids g l(-1)) closed-basin lake in the continental area of southwestern Greenland are described for the first time. Watercolumn data for every 5th consecutive day between April 20 and October 6, , and continuous recordings of lake water level and meteorological conditions are used to .
A simple model of runoff in West Greenland is proposed for the case that glaciers are in a state of balance. The independent variables in the model are estimated annual precipitation and evaporation while model parameters are evaluated by analysis of precipitation series from Greenland, and mass balance series from other parts of the world. Hydrological data collection in Greenland FIG.l Hydrological investigation sites in Greenland. be extrapolated to other areas in West Greenland. The measu rements will also be used to control the single parameters, precipitation gauges, wind velocities etc. Table 1 shows the various single parameters measured.
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The Mesozoic–Cenozoic separation of Greenland and North America produced the small oceanic basins of the Labrador Sea and Baffin Bay, connected via a complex transform system through the Davis Strait. During rifting and partial breakup sedimentary basins formed that record the changing regional sediment supply.
The onshore and offshore stratigraphy of Central West Greenland. HYDROLOGICAL PROCESSES Hydrol. Process. 23, – () Published online 22 May in Wiley InterScience () DOI: /hyp Hydrologic drainage of the Greenland Ice Sheet. Hydrological basins in West Greenland 51 original coding.
The original basin coding is here JHB G 05 0, i.e. Julianehâb district, fjord G from the south, 5th basin. The basins presented cover 86 km2, i.e. 83 per cent of the area of West Greenland, the remainder of the area being represented by steep slopes to the fjords. The Mesozoic-Cenozoic separation of Greenland Hydrological basins in West Greenland book North America produced the small oceanic basins of the Labrador Sea and Baffin Bay, connected via a complex transform system through the Davis Strait.
During rifting and partial breakup sedimentary basins formed that record the changing regional sediment supply. The onshore and offshore stratigraphy of Central West Greenland Author: Scott Jess, Alexander L. Peace, Christian Schiffer.
Tim Stott, Anne-Marie Nuttall, Eloise Biggs, Observed run-off and suspended sediment dynamics from a minor glacierized basin in south-west Greenland, Geografisk Tidsskrift-Danish Journal of Geography, /,2, (), ().
The Mesozoic–Cenozoic separation of Greenland and North America produced the small oceanic basins of the Labrador Sea and Baffin Bay, connected via a complex transform system through the Davis Strait.
During rifting and partial breakup sedimentary basins formed that record the changing regional sediment supply. The onshore and offshore stratigraphy of Central West Greenland.
The local glaciers in Greenland can easily be overlooked in the presence of the vast Greenland Ice Sheet (GIS) (see entry Greenland Ice Sheet).This is probably the main reason why relatively limited research has been conducted on these glaciers; despite they cover about 5–10% of the total ice cap and minor glacier area of the world (Weidick and Morris, ).
Predicting future hydrological regimes with regard to climate change is an increasingly important task for hydrologists. In polar regions the task is more difficult due to the lack of datasets and long term monitoring as well as logistical difficulties in remote and inaccessible basins.
Here, we demonstrate a case study predicting the future run-off in a difficult to model hydrological basin. State of Nevada Division of Water Resources. Last updated 8/12/ Acceptable Use Policy. Recommend this book. West Greenland. Hydrological Processes, 9, Observed run-off and suspended sediment dynamics from a minor glacierized basin in south-west Greenland.
Geografisk Tidsskrift- Danish Journal of Geography, DOI: / An endorheic basin (/ ˌ ɛ n d oʊ ˈ r iː. ɪ k /; also spelled endoreic basin or endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water, such as rivers or oceans, but converges instead into lakes or swamps, permanent or seasonal, that equilibrate through are also called closed or terminal basins.
BASINS was originally introduced in with subsequent releases in, The current version of BASINS was released in Sediment plumes as a proxy for local ice-sheet runoff in Kangerlussuaq Fjord, West Greenland - Volume 56 Issue - Daniel McGrath, Konrad Steffen, Irina Overeem, Sebastian H.
Mernild, Bent Hasholt, Michiel Van Den Broeke. The following models are available in BASINS Watershed Models: Hydrological Simulation Program - FORTRAN (HSPF) (U.S. EPA Supported) HSPF is a watershed model that simulates nonpoint source runoff and pollutant loadings for a watershed, combines these with point source contributions, and performs flow and water quality routing in reaches.
The seasonal cycle in the basin is characterized by a bimodal pattern of the rainfall distribution with maximum rainfall values in Mar., Apr., Oct., and Nov. (Beighley et al., ; Juarez, Robin, Li, Fu, & Fernandes, ).The rainy season in the north coincides with the dry season in the south and vice versa; so heavy rain in the north tends to compensate for light rain in the south.
In this preliminarily study, future () hydrological flows in a particular watershed (Shigar river at Shigar, ca. km2), nested within the upper Indus basin and fed by seasonal.
The mountains and fjords of Greenland preserve a record of nearly four billion years of Earth history - a story of mountain building, volcanic eruptions, primitive life and ice ages. During the vast period of time, through processes of continental drift, Greenland has journeyed from the southern hemisphere through the tropics to its present polar position.
Lundquist, D. Modelling runoff from a glacierized basin. Hydrological Aspects of Alpine and High Mountain areas. Proceedings of the Exeter Symposium, July IAHS Publication- Google Scholar. Quantifying supraglacial meltwater pathways in the Paakitsoq region, West Greenland CONRAD KOZIOL,1 NEIL ARNOLD,1 ALLEN POPE,2,3,4 WILLIAM COLGAN3,5 1Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, UK 2National Snow and Ice Data Center, University of Colorado, Boulder, CO, USA 3Cooperative Institute for Research in.
Imperial RIVER BASIN (chile) Hydrology Surface water. The headwaters of the Imperial River Basin are located to the west of the upper BioBio River Basin, from which it is separated by a series of mountain ranges, as Las Raíces and Sierra Nevada, which prevents taking advantage of water coming from the highest mountains.Drainage basins of the principal oceans and seas of the world.
Grey areas are endorheic basins that do not drain to the oceans. Ocean basins. The following is a list of the major ocean basins: About % of the world's land drains to the Atlantic Ocean.  In North America, surface water drains to the Atlantic via the Saint Lawrence River and Great Lakes basins, the.
Chemical Geology (Isotope Geoscience Section), () Elsevier Science Publishers B.V., Amsterdam [PD] Using stable isotopes as natural tracers to delineate hydrological drainage basins on the Greenland ice-sheet margin Niels Reeh" and Henrik Hojmark Thomsenb aDanish Polar Center, Strandgade H, DK Copenhagen K, Denmark bGeological Survey of Greenland.