scholarly journals Quantification of the ice-cored moraines' short-term dynamics in the high-Arctic glaciers Ebbabreen and Ragnarbreen, Petuniabukta, Svalbard

Geomorphology ◽  
2015 ◽  
Vol 234 ◽  
pp. 211-227 ◽  
Author(s):  
Marek W. Ewertowski ◽  
Aleksandra M. Tomczyk
Keyword(s):  
Polar Biology ◽  
2014 ◽  
Vol 37 (10) ◽  
pp. 1459-1468 ◽  
Author(s):  
Alison Beamish ◽  
Allison Neil ◽  
Ioan Wagner ◽  
Neal A. Scott

1972 ◽  
Vol 104 (6) ◽  
pp. 903-916 ◽  
Author(s):  
H. V. Danks ◽  
D. R. Oliver

AbstractThe diel periodicities of emergence of seven species of chironomids from two ponds in the Hazen Camp area (81°49′ N., 71°18′ W.) are considered in relation to physical factors. Emergence of all species is greatest during the middle part of the day: an increase in water temperature induces emergence and a decrease inhibits it, whereas changes in light intensity, ultraviolet radiation, sunshine, and wind appear to have no effect on the diel emergence pattern. In a shallow pond, males emerge slightly earlier in the day than females in some species. In the same pond also, emergence, particularly of females, is sometimes distinctly bimodal. In a deeper tarn where the diel temperature fluctuation is very small there is a single peak, which is less pronounced than in the shallow pond.That temperature controls the periodicity of emergence implies that short-term temperature changes which may inhibit adult activity are of great importance in the high arctic. At these latitudes, changes in light intensity evidently do not reliably indicate to the emerging organisms temperatures which fluctuate near critical thresholds for activity.


2017 ◽  
Vol 12 (2) ◽  
pp. 025001 ◽  
Author(s):  
Chelsea J Little ◽  
Helen Cutting ◽  
Juha Alatalo ◽  
Elisabeth J Cooper

2021 ◽  
Vol 11 (1) ◽  
pp. 154-160
Author(s):  
Andreas Alexander

Glacier cave visits are an important tourism activity on Svalbard with increasing popularity. This study investigates the thermal effect of touristic visits on the air temperature of a glacier cave on Longyearbreen, a small high-Arctic glacier. Short-term temperature perturbations of up to 1.59°C (42% local temperature increase) can be linked to human visitors. It is, however, unlikely that the local heat input from touristic visits is high enough to cause a lasting effect on the thermal regime of glacier caves and the surrounding ice.


2010 ◽  
Vol 88 (2) ◽  
pp. 170-177 ◽  
Author(s):  
Brage Bremset Hansen ◽  
Ronny Aanes ◽  
Bernt-Erik Sæther

Increased frequency of ground-icing events is likely to influence population dynamics in arctic ungulates, but their behavioural responses remain unexplored. During a record-mild winter with heavy rainfall, we analysed snow and ice characteristics and foraging trade-offs by Svalbard reindeer ( Rangifer tarandus platyrhynchus Vrolik, 1829) on a semi-isolated, recently occupied range. Snow depths were well within thresholds for cratering, but >90% of low altitudes was covered by a thick ice coat on the ground (median thickness 9 cm). Different strategies to cope with these conditions appeared. Part of the population sought mountainous habitat with very sparse vegetation. Individuals remaining at lower altitudes either used sparsely vegetated, wind-blown ridges partially covered with ice, or apparently applied olfactory senses to locate vegetation in ice-free microhabitat beneath the snowpack. No feeding craters were covered by ground ice, compared with most nearby controls. Following ground-ice avoidance, vegetation rather than snowpack properties determined fine-scale crater selection. Even under such poor conditions, the presence of medium- to high-quality forage (dwarf willow ( Salix polaris Wahlenb.) and fruticose lichens) rather than low-digestible, high-biomass forage (mosses) influenced cratering decisions. Behavioural plasticity combined with a gradually depleted lichen resource can partly buffer the reindeer against predicted climate change, at least in the short-term.


2017 ◽  
Author(s):  
Wenxin Zhang ◽  
Per-Erik Jansson ◽  
Bo Elberling

Abstract. Ecosystem CO2 fluxes in high Arctic are rather dynamic, as they are sensitive to climatic variability through multiple ecosystem processes, for instance, vegetation and snow dynamics as well as permafrost thawing, operating at different time scales. Uncertainties from both high-frequency measurements and model assumptions challenge model calibration to describe both short- and long-term phenomena related to weather and climate variabilities. In this study, we generated three model ensembles using a Monte-Carlo based uncertainty approach with acceptance criteria for 15 years of eddy covariance CO2 measurements of a high Arctic heath ecosystem based on the time-integrated CO2 fluxes within the day, the year and the entire period. The temporal distribution of residuals between the model and measurements indicated that the three model ensembles reasonably simulated diurnal, seasonal and long-term behaviours of CO2 fluxes respectively. The inter-annual variation of CO2 fluxes over 15 years showed the current ecosystem is at a transition from being a C sink to a C neutral balance. The long-term behaviour model ensemble simulated a more intensified diurnal C cycle than the short-term behaviour model ensembles. The intensified C cycle was mainly attributed to a faster depletion of the soil C pools. The sensitivities of posterior parameters to the model performance index (coefficient of determination, R2) reflected that parameters in the processes of soil water and heat transfer and snow dynamics regulated the short-term behaviour of CO2 fluxes, while parameters in the process of soil decomposition regulated the long-term behaviour of CO2 fluxes. Our results suggest that the development of ecosystem models should diagnose their effectiveness in capturing ecosystem CO2 exchange behaviour across different time scales. A clear trade-off may exist when the model is tuned to capture both the short- and long-term variation of CO2 fluxes. To constrain the model with the time-integrated CO2 fluxes is a simple and useful method to reduce the non-explained errors and to identify the crucial link to controlling parameters and processes.


2003 ◽  
Vol 34 (1-2) ◽  
pp. 51-70 ◽  
Author(s):  
Kathy L. Young ◽  
Ming-ko Woo

1998 was a very warm year for Canada and the High Arctic was no exception. A typical area was Resolute, Cornwallis Island, Nunavut, where the thaw season was extended and the thawing degree-days were larger than normal. The warm summer was accompanied by early spring melt and low rainfall. This study documents the thermo-hydrological responses including warming of the top soil, deepening of the active layer, alteration of the evaporation pattern, adjustment of the water table positions and runoff. The presence of semi-permanent snowbanks and patchy wetlands buffer some local sites from the warm and dry summer conditions. This and other studies show that the cryospheric and hydrologic systems may or may not recover quickly from the year to year variations in the climate, depending on how readily the storages (snow, ice and basin moisture) can be replenished. In view of the cumulative effects of storage depletion under climatic warming, short-term studies on thermo-hydrological behaviour in the Arctic provide a useful but insufficient analogue to capture the climatic change impacts.


1973 ◽  
Vol 30 (6) ◽  
pp. 717-723 ◽  
Author(s):  
G. F. Holeton

The routine of resting oxygen consumption of Arctic char (Salvelinus alpinus) from a high arctic lake (74°42′N) was measured at 2 (acclimated) and 6 C (unacclimated). The oxygen uptake versus wet weight relation at 2 C was: Log O2 uptake = 0.7316 Log weight – 1.0944. Oxygen uptake was low, not showing any evidence of "cold adaptation," and was comparable to projections of oxygen uptake versus temperature relations of other salmonid fish from lower latitudes.The short term metabolic response to a rise in temperature of 4 C was independent of body size except with fish with yolk sacs and weighing less than 0.125 g.


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