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  • 1
    Publication Date: 2020-07-07
    Description: The Filchner-Ronne Ice Shelf, fringing the southern Weddell Sea, is Antarctica's second largest ice shelf. At present, basal melt rates are low due to active dense water formation; however, model projections suggest a drastic increase in the future due to enhanced inflow of open-ocean warm water. Mooring observations from 2014 to 2016 along the eastern flank of the Filchner Trough (76°S) revealed a distinct seasonal cycle with inflow of Warm Deep Water during summer and autumn. Here we present extended time series showing an exceptionally warm and long inflow in 2017, with maximum temperatures exceeding 0.5°C. Warm temperatures persisted throughout winter, associated with a fresh anomaly, which lead to a change in stratification over the shelf, favoring an earlier inflow in the following summer. We suggest that the fresh anomaly developed upstream after anomalous summer sea ice melting and contributed to a shoaling of the shelf break thermocline.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 2
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    In:  EPIC3FRISP - Forum for Reasearch into Ice Shelf Processes, Gothenburg, 2016-10-04-2016-10-06
    Publication Date: 2019-08-19
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 3
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2017-12-06
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 4
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    In:  EPIC3EGU, General Assembly 2017, Vienna, 2017-04-24-2017-04-28
    Publication Date: 2019-10-04
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 5
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    Wiley
    In:  EPIC3Journal of Geophysical Research-Oceans, Wiley, 122(8), pp. 6437-6453, ISSN: 0148-0227
    Publication Date: 2019-10-04
    Description: New two-year long records from three moorings, located at 76°S along the eastern flank and shelf of the Filchner Trough, give insight in the seasonal cycle of hydrography to a region where Modified Warm Deep Water (MWDW) enters the southern Weddell Sea continental shelf, possibly reaching the Filchner Ronne Ice Shelf, the biggest ice shelf (by volume) in Antarctica. A persistent northward flow of Ice Shelf Water (ISW) is found along the slope of the trough at 600 m depth, while the data on the shelf indicate a seasonal cycle, characterized by four phases. A distinct warm inflow period (separated in two phases), with maximum temperatures of −1°C, appears to be related to the seasonal heaving of the Antarctic Slope Front thermocline along the continental shelf break further north and a seasonal extension of the ISW layer onto the Eastern Shelf. The density gradients between the ISW in the trough and the MWDW on the adjacent shelf drive the southward flow during these phases. A flow reversal is found in winter, ceasing the southward flow along the eastern flank of the trough. Weaker density gradients between the trough and the shelf during winter allow a westward flow, partly driven by a N-S density gradient, existing across the Eastern Shelf during this time. From spring through to summer the ISW layer in the trough extends onto the eastern shelf where it occupies the bottom layer at our moorings and it is associated with northward flow.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 6
    Publication Date: 2019-04-30
    Description: The Filchner-Ronne Ice Shelf (FRIS), fringing the southern Weddell Sea, plays a key role in the formation of Weddell Sea Deep and Bottom Water, which are precursors of world ocean’s AABW. At present, a large continental shelf covered with cold and dense water protects FRIS from intense basal melting. Model studies, however, have suggested the potential for enhanced flow of Modified Warm Deep Water (MWDW) toward and under FRIS via the Filchner Trough, causing a substantial increase in basal melt rates by the end of this century. Mooring time series spanning 2014 to 2016 at 76 ◦ S revealed a distinct seasonal cycle in hydrography along the eastern flank of the Filchner Trough with warm inflow occurring only during summer, while winter is dominated by a weakly stratified water column at the surface freezing point. The seasonality is driven by seasonal evolution of the shelf break thermocline in combination with local buoyancy forcing. The mooring time series was extended to 2018 and while the general pattern of the described seasonal cycle is reaffirmed, an unprecedented strong warm inflow with temperatures being about 0.5 ◦ C above the previously observed inflow, was observed in 2017. Additionally, bottom temperatures above −1.5 ◦ C persisted throughout the whole winter together with a fresh anomaly in salinity. A warm signal was also measured by a LoTUS buoy deployed at 77 ◦ C during 2017. Weaker than average along-coast wind stress was present in the upstream region from summer through winter 2017 and likely lead to a stronger shoaling of the shelf break thermocline upstream of Brunt Shelf Ice causing the observed inflow. Likely, MWDW also entered the Brunt Ice Shelf cavity, which lead to enhanced basal melting that, in turn, could explain the observed fresh water anomaly. The inflow event affected the continental shelf hydrography in a favourable way for an earlier onset of warm inflow in the following summer.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 7
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    Geophysical Institute, University of Bergen
    In:  EPIC3Bergen, Geophysical Institute, University of Bergen
    Publication Date: 2015-10-13
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 8
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2014. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 119 (2014): 228-240, doi:10.1002/2013JC009437.
    Description: The narrow and deep Faroe Bank Channel (FBC) is an important pathway for cold, dense waters from the Nordic Seas to flow across the Iceland-Scotland ridge into the North Atlantic. The swift, turbulent FBC overflow is associated with strong vertical mixing. Hydrographic profiles from a shipboard survey and two Slocum electric gliders deployed during a cruise in May–June 2012 show an intermediate water mass characterized by low salinity and low oxygen concentration between the upper waters of Atlantic origin and the dense overflow water. A weak low-salinity signal originating north-east of Iceland is discernible at the exit of the FBC, but smeared out by intense mixing. Further west (downstream) marked salinity and oxygen minima are found, which we hypothesize are indicators of a mixture of Labrador Sea Water and Intermediate Water from the Iceland Basin. Water mass characteristics vary strongly on short time scales. Low-salinity, low-oxygen water in the stratified interface above the overflow plume is shown to move along isopycnals toward the Iceland-Faroe Front as a result of eddy stirring and a secondary, transverse circulation in the plume interface. The interaction of low-salinity, low-oxygen intermediate waters with the overflow plume already at a short distance downstream of the sill, here reported for the first time, affects the final properties of the overflow waters through entrainment and mixing.
    Description: This work was funded by the Research Council of Norway, through the FRINAT program, under the project 204867/V30, ‘‘Faroe Bank Channel Overflow: Dynamics and Mixing.’’
    Description: 2014-07-10
    Keywords: Faroe Bank Channel ; North Atlantic ; Overflow ; Water masses
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 9
    Publication Date: 2022-05-25
    Description: Author Posting. © Elsevier B.V., 2008. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Deep Sea Research Part I: Oceanographic Research Papers 55 (2008): 737-750, doi:10.1016/j.dsr.2008.02.007.
    Description: The continental slopes in the oceans are often covered by small-scale topographic features such as submarine canyons and ridges. When dense plumes, flowing geostrophically along the slope, encounter such features they may be steered downslope inside and alongside the topography. A set of laboratory experiments was conducted at the rotating Coriolis platform to investigate the effect of small-scale topography on plume mixing. A dense water source was placed on top of a slope, and experiments were repeated with three topographies: a smooth slope, a slope with a ridge, and a slope with a canyon. Three flow regimes were studied: laminar, waves, and eddies. When a ridge or a canyon were present on the slope, the dense plume was steered downslope and instabilities developed along the ridge and canyon wall. This happened regardless of the flow characteristics on the smooth slope. Froude and Reynolds numbers were estimated, and were found to be higher for the topographically steered flow than for flow on smooth topography. The stratification in the collecting basin was monitored and the mixing inferred. The total mixing and the entrainment rate increased when a ridge or a canyon were present. The difference in mixing levels between the regimes was smaller when topography was present, indicating that it was the small-scale topography and not the large-scale characteristics of the flow that determined the properties of the product water.
    Description: AW was funded by the Swedish Research Council and ED in part by Meltzer Stiftelsen, for which we are grateful. CC was supported by an NSF grant OCE-0085089. The work described in this publication was supported by the European Community's Sixth Framework Programme through the grant to the budget of the Integrated Infrastructure Initiative HYDRALAB III, Contract no. 022441 (RII3).
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
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  • 10
    Publication Date: 2021-10-13
    Description: The Filchner-Ronne Ice Shelf, fringing the southern Weddell Sea, is Antarctica's second largest ice shelf. At present, basal melt rates are low due to active dense water formation; however, model projections suggest a drastic increase in the future due to enhanced inflow of open-ocean warm water. Mooring observations from 2014 to 2016 along the eastern flank of the Filchner Trough (76°S) revealed a distinct seasonal cycle with inflow if Warm Deep Water during summer and autumn. Here we present extended time series showing an exceptionally warm and long inflow in 2017, with maximum temperatures exceeding 0.5°C. Warm temperatures persisted throughout winter, associated with a fresh anomaly, which lead to a change in stratification over the shelf, favoring an earlier inflow in the following summer. We suggest that the fresh anomaly developed upstream after anomalous summer sea ice melting and contributed to a shoaling of the shelf break thermocline.
    Keywords: 551.46 ; ocean-ice shelf interaction ; Weddell Sea ; warm inflow ; Antarctic Slope Front ; Filchner-Ronne Ice Shelf
    Language: English
    Type: map
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