If I may add one more speculative question: are the portions of glacial sheets formed during periods of
high ice flux less stable, and more prone to calving, than those formed during slow flux?
Not exact matches
However,
ice is a poor conductor so, unless
ice is very thin or the geothermal heat
flux very
high, tends not to influence melt at the
ice surface.
Thus, for every 1 % increase in local sea level, there is a ~ 5 % increase in
ice flux through the grounding line (though this may be
higher if the bed is slippery near the grounding line, see Tsai et al. 2015).
«In addition, we are currently developing a method that also allows for
high - precision hydrogen isotopic measurements on methane in
ice cores, which will further improve our emission
flux constraints,» revealed Fischer.
Numerous recent studies based on both observations and model simulations indicate that reduced Barents - Kara sea
ice in late fall favors a strengthened and northwestward expansion of the Siberian
high, increased poleward heat
flux, weakened polar vortex, and ultimately a negative AO.
Therefore the sea
ice products and
High Latitude SST and
Flux products were unavailable through FTP.
The Younger Dryas appears to have been triggered by
high latitude meltwater
flux from the NH
ice sheet interrupting deep water formation and halting the AMOC.
Link to paper:
High geothermal heat
flux in close proximity to the Northeast Greenland
Ice Stream
Even simply measuring net
flux of energy into the Arctic via ocean currents from record
high OHC would call into serious question the possibility that the long term decline in Arctic sea
ice would reverse or «revert to the mean».
Ice significantly reduces the heat
flux between ocean and atmosphere; through its
high albedo it has a strong influence on the radiation budget of the entire Arctic.
See lower figure 5.7 total heat
flux is essentially zero
higher than 80 north and very little down to 70 north outside winter sea
ice extent.
Sea
Ice products (last 31 days)(ftp://osisaf.met.no/prod/
ice/) Sea
Ice product archive (ftp://osisaf.met.no/archive/
ice/) Atlantic
High Latitude SST products (last 31 days)(ftp://osisaf.met.no/prod/sst/) Atlantic
High Latitude SST product archive (ftp://osisaf.met.no/archive/sst/) Atlantic
High Latitude
Flux products (last 31 days)(ftp://osisaf.met.no/prod/
flux/) Atlantic
High Latitude
Flux product archive (ftp://osisaf.met.no/archive/
flux/)
«As a result, the loss of glacier mass worldwide, along with the corresponding release of carbon, will affect
high latitude marine ecosystems, particularly those surrounding the major
ice sheets that now receive fairly limited land - to - ocean
fluxes of carbon.»
This report discusses our current understanding of the mechanisms that link declines in Arctic sea
ice cover, loss of
high - latitude snow cover, changes in Arctic - region energy
fluxes, atmospheric circulation patterns, and the occurrence of extreme weather events; possible implications of more severe loss of summer Arctic sea
ice upon weather patterns at lower latitudes; major gaps in our understanding, and observational and / or modeling efforts that are needed to fill those gaps; and current opportunities and limitations for using Arctic sea
ice predictions to assess the risk of temperature / precipitation anomalies and extreme weather events over northern continents.
High - latitude ocean and sea
ice surface
fluxes: challenges for climate research.
Caused by
ice formation resulting from a change in heat transport triggered by meltwater
flux at
high NH latitude initiated by orbital forcing; --RRB-
The US CLIVAR
High Latitude Surface
Flux Working Group was formed in January 2008, with the particular goal of addressing some of the challenges associated with air - sea and air -
ice - ocean exchanges in Arctic, Antarctic, and Southern Ocean regions.