4.7 Article

On the seasonal freshwater stratification in the proximity of fast-flowing tidewater outlet glaciers in a sub-Arctic sill fjord

期刊

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
卷 118, 期 3, 页码 1382-1395

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/jgrc.20134

关键词

-

资金

  1. Commission for Scientific Research in Greenland (KVUG)
  2. Danish Agency for Science, Technology, and Innovation
  3. Danish Energy Agency
  4. Aage V. Jensen Charity Foundation
  5. National Science Foundation [NSF-OPP 0909552, 0909333]
  6. Canada Excellence Research Chair (CERC) Program
  7. Office of Polar Programs (OPP)
  8. Directorate For Geosciences [0909552] Funding Source: National Science Foundation

向作者/读者索取更多资源

The Greenland Ice Sheet releases large amounts of freshwater into the fjords around Greenland and many fjords are in direct contact with the ice sheet through tidewater outlet glaciers. Here we present the first seasonal hydrographic observations from the inner part of a sub-Arctic fjord, relatively close to and within 4-50 km of a fast-flowing tidewater outlet glacier. This region is characterized by a dense glacial and sea ice cover. Freshwater from runoff, subglacial freshwater (SgFW) discharge, glacial, and sea ice melt are observed above 50-90m depth. During summer, SgFW and subsurface glacial melt mixed with ambient water are observed as a layered structure in the temperature profiles below the low-saline summer surface layer (<7 m). During winter, the upper water column is characterized by stepwise halo-and thermoclines formed by mixing between deeper layers and the surface layer influenced by ice melt. The warm (T>1 degrees C) intermediate water mass is a significant subsurface heat source for ice melt. We analyze the temperature and salinity profiles observed in late summer with a thermodynamic mixing model and determine the total freshwater content in the layer below the summer surface layer to be between 5% and 11%. The total freshwater contribution in this layer from melted glacial ice was estimated to be 1-2%, while the corresponding SgFW was estimated to be 3-10%. The winter measurements in the subsurface halocline layer showed a total freshwater content of about 1% and no significant contribution from SgFW.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

Article Oceanography

An Updated View on Water Masses on the pan-West Greenland Continental Shelf and Their Link to Proglacial Fjords

S. Rysgaard, W. Boone, D. Carlson, M. K. Sejr, J. Bendtsen, T. Juul-Pedersen, H. Lund, L. Meire, J. Mortensen

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2020)

Article Oceanography

Subglacial Discharge and Its Down-Fjord Transformation in West Greenland Fjords With an Ice Melange

John Mortensen, Soren Rysgaard, Jorgen Bendtsen, Kunuk Lennert, Torsten Kanzow, Henrik Lund, Lorenz Meire

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2020)

Article Oceanography

Vertical Mixing in Stratified Fjords Near Tidewater Outlet Glaciers Along Northwest Greenland

Jorgen Bendtsen, Soren Rysgaard, Daniel F. Carlson, Lorenz Meire, Mikael K. Sejr

Summary: Research has shown that near tidewater outlet glaciers, localized mixing hot spots can significantly contribute to vertical exchange, especially due to the position of these glaciers near the outlets, leading to the formation of this type of localized mixing.

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2021)

Article Oceanography

Seasonal Hydrography of Ameralik: A Southwest Greenland Fjord Impacted by a Land-Terminating Glacier

A. E. Stuart-Lee, J. Mortensen, A. S. van der Kaaden, L. Meire

Summary: The study focuses on the seasonal hydrography of Ameralik, a Greenlandic fjord impacted by a land-terminating glacier. The absence of subglacial discharge and glacial ice in Ameralik significantly affects the inner fjord density profiles and circulation. During the summer, a large fraction of meltwater is retained within the fjord, while substantial freshwater export occurs during winter coastal inflows.

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2021)

Article Oceanography

Multidecadal Water Mass Dynamics on the West Greenland Shelf

J. Mortensen, S. Rysgaard, M. H. S. Winding, T. Juul-Pedersen, K. E. Arendt, H. Lund, A. E. Stuart-Lee, L. Meire

Summary: The waters on the West Greenland continental shelf and slope, particularly the Baffin Bay Polar Water (BBPW), have significant impacts on the global climate system and the Greenland Ice Sheet. This study examines the frequency of BBPW reaching the southern part of West Greenland at approximately 64 degrees N, and its association with temperature changes. The findings suggest that BBPW plays a crucial role in the interpretation of temperature changes and the melt of the Greenland Ice Sheet.

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2022)

Article Biodiversity Conservation

Distinct latitudinal community patterns of Arctic marine vertebrates along the East Greenlandic coast detected by environmental DNA

Mads Reinholdt Jensen, Signe Hogslund, Steen Wilhelm Knudsen, Julius Nielsen, Peter Rask Moller, Soren Rysgaard, Philip Francis Thomsen

Summary: The study aims to investigate the transition in fish and marine mammal communities from South to Northeast Greenland using environmental DNA (eDNA). The results demonstrate a clear shift in biological communities from south to northeast, with different fish and mammal species dominating each region. The study highlights the potential of eDNA sampling in detecting latitudinal changes in marine biological communities and its feasibility in remote areas as climate change progresses.

DIVERSITY AND DISTRIBUTIONS (2023)

Article Environmental Sciences

Coastal freshening drives acidification state in Greenland fjords

Henry C. Henson, Johnna M. Holding, Lorenz Meire, Soren Rysgaard, Colin A. Stedmon, Alice Stuart-Lee, Jorgen Bendtsen, Mikael Sejr

Summary: Greenland's fjords and coastal waters are highly productive and sustain important fisheries, but retreating glaciers and increasing meltwater are changing fjord circulation and biogeochemistry, potentially threatening future productivity. The freshening of Greenland fjords caused by unprecedented melting of the Greenland Ice Sheet may alter carbonate chemistry in coastal waters, impacting CO2 uptake and causing acidification-related biological consequences. However, there have been few studies on the current acidification state in Greenland coastal waters.

SCIENCE OF THE TOTAL ENVIRONMENT (2023)

Article Marine & Freshwater Biology

Influence of glacier type on bloom phenology in two Southwest Greenland fjords

A. E. Stuart-Lee, J. Mortensen, T. Juul-Pedersen, J. J. Middelburg, K. Soetaert, M. J. Hopwood, A. Engel, L. Meire

Summary: The release of meltwater from marine-terminating glaciers influences primary production in fjords along Greenland's coastline. However, it is still unclear how local ecosystems will adapt and how it will affect hydrography as these glaciers retreat onto land. In this study, we examined how marine- and land-terminating glaciers respectively influence bloom dynamics in two fjords in west Greenland.

ESTUARINE COASTAL AND SHELF SCIENCE (2023)

Article Oceanography

An Updated View of the Water Masses on the Northeast Greenland Shelf and Their Link to the Laptev Sea and Lena River

E. W. Willcox, J. Bendtsen, J. Mortensen, C. Mohn, M. Lemes, T. J. Pedersen, J. Holding, E. F. Moller, M. K. Sejr, M. S. Seidenkrantz, S. Rysgaard

Summary: This study presents a synoptic survey of the Northeast Greenland shelf and slope during late summer 2017, investigating hydrography, nutrients, conservative tracers, and climate factors. The results indicate that the Laptev Sea is a major freshwater source in the region during this period, and there is no conclusive evidence of Pacific Water. The observations suggest a direct link between Northeast Greenland hydrology and processes occurring on Eurasian shelves.

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2023)

Article Oceanography

Distinguishing Physical and Biological Controls on the Carbon Dynamics in a High-Arctic Outlet Strait

T. M. Burgers, L. A. Miller, S. Rysgaard, J. Mortensen, B. Else, J. -E Tremblay, T. Papakyriakou

Summary: In August 2014, we characterized the physico-chemical properties of water masses entering Nares Strait. We used an extended OMP analysis to estimate mixing fractions and determine the role of physical and biological processes in the distribution of DIC. Our observations include evidence of Siberian shelf waters and diluted Pacific-origin upper halocline layer entering Nares Strait. These mixed-origin water masses drive phytoplankton bloom in Kane Basin, leading to decreased surface pCO(2) concentrations. The positioning of the Transpolar Drift and the balance of Atlantic and Pacific water delivered to Nares Strait play an important role in regional biological productivity and carbon uptake.

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2023)

Article Geosciences, Multidisciplinary

Glacier retreat alters downstream fjord ecosystem structure and function in Greenland

Lorenz Meire, Maria Lund Paulsen, Patrick Meire, Soren Rysgaard, Mark James Hopwood, Mikael Kristian Sejr, Alice Stuart-Lee, Koen Sabbe, Willem Stock, John Mortensen

Summary: Glacier retreat in Greenland alters the primary productivity, ecosystem structure, and functioning of downstream fjord ecosystems. Monthly sampling in two fjords in southwest Greenland in 2016 revealed that subglacial discharge from marine-terminating glaciers sustains high phytoplankton productivity dominated by diatoms and grazed by larger mesozooplankton throughout summer. On the other hand, melting of land-terminating glaciers results in a fjord ecosystem dominated by bacteria, picophytoplankton, and smaller zooplankton, with only one-third of the annual productivity and half the CO2 uptake compared to the fjord downstream from marine-terminating glaciers.

NATURE GEOSCIENCE (2023)

暂无数据