Helmholtz Infrastructure Initiative FRAM ( Fr ontiers in A rctic Marine M onitoring). The long-term observatory Hausgarten is a network of twenty stations in the Fram Strait, whose coordinates are re-visited
Research (AWI) laid the “foundation stone” for a unique long-term observatory in the partly ice-covered Fram Strait between Greenland and Svalbard, which they call their HAUSGARTEN. The deep-sea observatory
Arctic, which will grow thicker as the winter progresses. One year later, we should have reached the Fram Strait between Greenland and Svalbard. In the course of that year, a total of 600 people will take
studies at a major long-term monitoring station in the Arctic: the AWI’s Hausgarten observatory in the Fram Strait, where experts from various disciplines are investigating all aspects of the ecosystem, from
atmospheres FESOM 1.4 and FESOM 2.0 Mesh refinement in FESOM2 Wekerle et al., 2017 Eddy resolving in the Fram Strait Wekerle et al., 2017 Wekerle et al., 2017 Global FESOM2 setup with 4.5 km Arctic Ocean Sea
data P*(x) k2(x) kT(x) P*(x) k2(x) Presentation Title | 22U.S. Naval Research Laboratory Future plans Fram 1893-1996 www.mosaic-expedition.org Beaufort Sea Moorings (USA), ~10 years www.whoi
layer (e.g. Barents Sea) T2m warming signal SCDA highly beneficial in Barents Sea, but worse south of Fram Strait Arctic basin May SIT correlated with Sep SIC (Bushuk et al., 2017) hydrography Reduces bias(SIT)
and reanalysis), so difficult to repond in short. A lso such studies are ongoing now in the Y O P P fram ew ork. I w ill try to list at least som e points: • There is a gap of inform ation on w ind, tem
impact on the turbulent fluxes. Our first analysis shows only weak impact of clouds over the open Fram Strait during strong convection, but – dependent on the optical thickness of the clouds – moderate
outbreaks over Fram Strait. One of our goals is to compare in situ measurements with satellite measurements and we could manage this week one flight following exactly the track of CloudSat over Fram Strait. This