2 edition of satellite-based study of sea ice dynamics in the Central Canadian Arctic Archipelago found in the catalog.
satellite-based study of sea ice dynamics in the Central Canadian Arctic Archipelago
J. R. Marko
Bibliography: p. 105.
|Statement||by J. R. Marko.|
|Series||Contractor report series -- 77-4., Contractor report series (Institute of Ocean Sciences, Patricia Bay) -- no. 77-4.|
|Contributions||Institute of Ocean Sciences, Patricia Bay.|
|The Physical Object|
|Pagination||xi, 106 p. :|
|Number of Pages||106|
Christie L. Logvinova, Karen E. Frey, Paul J. Mann, Aron Stubbins and Robert G. M. Spencer, Assessing the potential impacts of declining Arctic sea ice cover on the photochemical degradation of dissolved organic matter in the Chukchi and Beaufort Seas, Journal of Geophysical Research: Biogeosciences, , 11, (), ().Cited by: At the height of the last ice age, when Chicago was buried under a mile-deep sheet of ice, global temperatures averaged just 5°C (9°F) cooler than today. From historical weather-station data the global average temperature is already +°C warmer than in Arrhenius’ time, . His research interests span a broad range of areas including the ocean, atmosphere, sea-ice and land, and their interactions relating to climate. He is particularly interested in understanding the dynamics of air-sea coupled feedback on the oceanic mesoscale (km) and submeso-scale (km) regimes. from the ice divide with the Institute Ice Stream. The lake is approximately 15 km long and over 3 km across at its widest point. Seismic surveys have revealed that the lake is over m deep in places. The ice sheet above the lake isbetweenandkmthick,withthelakesurfaceover 1 km beneath present sea level within a distinct topo-.
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Get this from a library. A satellite-based study of sea ice dynamics in the Central Canadian Arctic Archipelago. [J R Marko; Institute of Ocean Sciences, Patricia Bay,].
Furthermore, in the central Canadian Arctic Archipelago, elevated IP 25 values indicate relatively more intensive spring sea-ice occurrences, beginning at ca. – cal. yr BP (Belt et al.
Marko, J.R. () A Satellite-based Study of Sea Ice Dynamics in the Central Canadian Arctic Archipelago. Contractor Report Series No. 77–4, pp.
Institute of Ocean Sciences, Sidney, Canada, V8L 4B2 Google ScholarCited by: Detection of melt onset over the northern Canadian Arctic Archipelago sea satellite-based study of sea ice dynamics in the Central Canadian Arctic Archipelago book from RADARSAT, – Article in Remote Sensing of Environment June with Reads.
Cheng, B. (), On the modelling of sea ice thermodynamics and air‐ice coupling in the Bohai Sea and the Baltic Sea, Tech. Rep. 5, Finnish Inst. of Marine Res., Helsinki. Google Scholar Chernoff, H.
(), A measure of asymptotic efficiency for tests of a hypothesis based on the sum of observations, Ann. Math. statis., 23 (4), Satellite-based Estimates of Sea Ice Volume Flux: Applications to the Fram Strait Region - Dr. Gunnar Spreen - Doctoral Thesis / Dissertation - Geography / Earth Science - Physical Geography, Geomorphology, Environmental Studies - Publish your bachelor's or.
The thickness of old level ice was reduced by 32 % between the s and ; The relative amount of ridged ice was reduced by 50% between the s and ; The ice cover remains preconditioned for new summers of minimum sea ice extent.
Introduction. The Arctic Ocean has undergone unprecedented changes in sea ice extent and thickness in recent decades, with old, stable multi-year ice (MYI) being largely replaced by young, thinner first-year ice satellite-based study of sea ice dynamics in the Central Canadian Arctic Archipelago book (Maslanik et al.,Stroeve et al., ).These changes, which have been particularly pronounced in the Beaufort and Chukchi seas (Meier et al.,Douglas, Cited by: 1.
Introduction. Climate-driven alterations of the environment are fastest and deepest in the Arctic Ocean (), where warming, acidification, the demise of sea ice and ensuing changes in freshwater balance and upper ocean dynamics impact the marine ecosystem in different concurrent ways ().At the lowest level of the food web, the photosynthetic primary production (PP) of organic matter (OM) by Cited by: The reduction in sea ice and warming of Arctic sea waters also has changed circum-arctic vegetation although the patterns are complex: a satellite-based measure of plant greening (NDVI) increased during –, suggesting an earlier green-up of the vegetation but then NDVI declined from – (Bhatt et al.
Strong linkage of ice-edge dynamics and air–sea heat fluxes (and SAT, not shown; e.g., Overland et al. ) is evident from Fig. The SAT increase due to ice–albedo satellite-based study of sea ice dynamics in the Central Canadian Arctic Archipelago book may be traced up to several hundred kilometers from the ice edge into the interior of the Siberian region, as evident from Fig.
by: Jeffries, M.O., K. Morris, and C.R. Duguay, "Floating ice: lake ice and river ice", Satellite Image Atlas of Glaciers of the World – State of the Earth’s Cryosphere at the Beginning of the 21st Century: Glaciers, Global Snow Cover, Floating Ice, and Permafrost and Periglacial Environments: U.S.
Geological Survey Professional Paper A, pp. AA, Fast ice (also called land-fast ice, landfast ice, and shore-fast ice) is sea ice that is "fastened" to the coastline, to the sea floor along shoals or to grounded icebergs.
New!!: Sea and Fast ice See more» Fathom. A fathom is a unit of length in the imperial and the U.S. customary systems equal to, used especially for measuring the depth. Recently, however, there has been significant arctic warming, accompanied by changes in the extent, thickness distribution, and properties of the arctic sea ice cover.
The need to understand these changes and their impact on arctic stratification and circulation, sea ice evolution, and the acoustic environment motivate this initiative.
Cazenave, N.M. Mognard, W. Llovel, and F. Frappart,Satellite-based high latitude snow and C. Labine,Sharply increased mass loss from glaciers and ice caps in the Canadian Arctic Archipelago, Nature,W.,Postglacial variations in the level of the sea: Implications for climate dynamics and solid-earth.
The coastlines of the Canadian Archipelago, Greenland and Svalbard are considered stable due to their predominantly rocky nature, the persistence of sea ice throughout the summer season (for the Canadian Archipelago) and because of a strong post-glacial rebound (rise of Cited by: On the surface, this appears to disagree with my measurement above that Arctic Basin ice area is greater than The difference is that I am only considering regions that have perennial ice – i.e my PIPS calculations assume that there is no summer ice in Hudson Bay or the Barents Sea, and that they are a “don’t care” for estimating minimum extent.
Fig. The USCGC (Coast Guard Cutter) Bear moored to sea ice in The Bear was initially purchased by the Navy for the Greely Relief Expedition in (Schley ) and subsequently served with the Revenue Cutter Service/Coast Guard in Alaska untilthen on Admiral Byrd’s expeditions to Antarctica from toand finally with the Navy on the Greenland Patrol during World Author: John E.
Walsh, David H. Bromwich, James. Overland, Mark C. Serreze, Kevin R. Wood. Sea ice cover in the Arctic and Antarctic is an important indicator of changes in the climate, with important environmental, economic and security consequences. The complexity of the spatio-temporal dynamics of sea ice makes it difficult to assess the temporal nature of the changes - e.g.
linear or exponential - and their precise geographical : James Hogg, Maria Fonoberova, Igor Mezic. Active-layer soil moisture content regional variations in Alaska and Russia by ground-based and satellite-based methods, through Implications of Arctic Sea Ice Decline for the Earth System.
Canadian Arctic Archipelago. Evansia, (3) The following is a partial list of publications which have used data from the Ocean Productivity site. Deep Sea Research Part I: Oceanographic Research Papers, Satellite-based decadal change assessments of pan-Arctic environments. Living coccolithophores community from Southern Tyrrhenian Sea (Central Mediterranean — Summer ).
Actual and insolation-weighted Northern Hemisphere snow cover and sea-ice between Climate Dynamics, 22, So it appears Dr. Pielke Sr could help with pre Arctic sea ice data, possibly NOAA satellite data.
Active layer dynamics on Central Yamal, Russia due to climatic fluctuations. In: P. Deline, X. Bodin and L. Ravanel (eds.), 5th European Conference on Permafrost - Book of Abstracts, 23 June-1 July, Chamonix, France.
This chapter describes the infrastructure and approach needed to create an Arctic Observing Network (AON), including ideas on types, number, and distribution of network components; where observations might be effectively made; and the role that remote sensing and novel technologies might play.
This review includes the blue‐shaded Ocean area that is north of Fram Strait and the Canadian Archipelago (i.e., we do not consider the Bering Sea, Hudson Bay, and the Nordic Seas in this study).
The green area depicts the circumpolar land area north of 45° N, for which this review considers the pan‐arctic terrestrial C by: The EAT the North America Arctic Transect (NAAT) (Fig. 1) are well situated to examine two areas of the Arctic that are most strongly affected by rapid sea-ice changes, the Beaufort Sea in the in the vicinity of the NAAT and the Barents/ West Kara seas in the vicinity of the EAT (Fig.
4a & b). Sea-ice melt CO2-carbonate chemistry in the western Arctic Ocean: meltwater contributions to air-sea CO2 gas exchange, mixed-layer properties and rates of net community production under sea ice. Biogeosciences. 11(23), doi: /bg.
Managing Degraded OHV Trails in the Arctic Parklands Blain C. Anderson 1, Kevin G. Meyer 2 1 National Park Service, Alaska Regional Office, W. 5th Ave., Anchorage, AK,USA, [email protected] 2 National Park Service, W.
5th Ave., Anchorage, AK,USA, [email protected] Alaska's National Parklands in the arctic have struggled. Forty years ago, climate scientists predicted the Arctic to be one of Earth’s most sensitive climate regions and thus extremely vulnerable to increased CO2.
The rapid and unprecedented changes observed in the Arctic confirm this prediction. Especially significant, observed sea ice loss is altering the exchange of mass, energy, and momentum between the Arctic Ocean and by: Temporal and spatial variations of air-sea CO2 fluxes in the Canadian Arctic Archipelago.
Ahmed, Mohamed (1) (Presenter), T. Papakyriakou (2) and B. Else. We froze our research vessel Lance into the sea ice in the Arctic Ocean north of Svalbard and let it drift from January to June to study the thin sea ice system. American Libraries Canadian Libraries Universal Library Community Texts Project Gutenberg Biodiversity Heritage Library Children's Library.
Open Library. Books by Language Additional Collections. Featured movies All video latest This Just In Prelinger Archives Democracy Now. Full text of "Oceanus". Su J Wu HD Zhang YF et al.
A coupled ice-ocean model for the Bohai Sea - I. Study on model and parameter Acta Oceanol. Sin. 23 (4) Middleton J. The coastal-trapped wave paddle and open boundary conditions Ocean Modelling 12() JANUARYAlaska Marine Science Symposium Gerry Sanger Andrew Trites Alexandra Ravelo Simone Welch HOTEL CAPTAIN COOK & EGAN CENTER • ANCHORAGE, ALASKA S.
Ulrich SHOWCASING MARINE RESEARCH IN THE ARCTIC OCEAN, BERING SEA, AND GULF OF ALASKA Alaska Marine Science Symposium Book of Abstracts. Sea ice dynamics were related to polar bear Delta13C, suggesting that the bears' diets shift in response to environmental change. Overall, these results highlight the biological link between polar bears and ringed seals, as well as sea ice dynamics, and the importance of considering geographic location in stable isotope studies.
(Au) I, G. Arctic weather and sea ice information infrastructures: dynamics and drivers In ArcticInfo a team of social scientists, meteorologists and sea ice experts study. Full text of "Oceanus" See other formats REPORTS ON RESEARCH AT THE WOODS HOLE OCEANOGRAPHIC INSTITUTION Volume:)7, Number 2 Fall WHOI Science at the Top of the World \JC\M REPORTS ON RESEARCH AT THE WOODS HOLE OCEANOGRAPHIC INSTITUTION Vol.
37, No. 2 Fall ISSN Arctic Research Human ivxt'a niters share their arctic space. and sea ice melt in the Arctic Ocean range between several years to centuries.
The multi-model average forecast based on models participating in the Intergovernmental Panel for Climate Change Fourth Assessment Report (IPCC-AR4) suggest a 50% or more reduction of summer sea ice cover in the Arctic Ocean by the end of this Size: 3MB.
To study changes in sea ice characteristics indicative of ringed seal habitat (and linked, through predator/prey relationships, to polar bear habitat), we examined historical changes in sea ice concentration and type within M'Clintock Channel and the Gulf of Boothia, two regions of the Canadian Arctic Archipelago, during The Canadian High Arctic has been warming for several decades and is predicted to undergo substantially more warming over the next century.
Increased temperatures are expected to alter the composition, structure, and function of Arctic plant communities. To better understand High Arctic tundra responses to climate warming, I conducted longitudinal and experimental studies in a snowbed heath.
The Atlantic pdf Space Workshop assessed opportunities for EO research and development, pdf activities and ICT evolution, with a specific focus on the Atlantic region, which will be the basis for future ESA investments, addressing key information needs of this important area in the context of the ESA EO Atlantic Regional Initiative.online version of the program book.
Please click the following link to download and install: When you are finished installing, please return to this window and PRESS. Ebook this year, Stein et al., published a ebook of Arctic sea ice variations throughout the Holocene that appeared to establish that there is more Arctic sea ice now than for nearly all of the l years.
The study region, the Chukchi Sea, was deemed representative of most of the Arctic, as the authors asserted that “the increase in sea ice extent during the late.