gradient of +0.5 K/100 m approximately 100 km west of measuring site extending from north of the Fram Street to Janindicates a stable stratification. Below 750 m, the vertical profile of relative humidity

Press release

Press release

Research Conference, Barcelona, Spain, 17 November 2014 - 21 November 2014 . 8. Schewe, I. , FRAM-Konsortium (2014): FRAM: A multidisciplinary observatory in the North Atlantic - Arctic Ocean transition zone [...] HAUSGARTEN (Fram Strait) , Deep Sea Research I, 58 (11), pp. 1069-1083 . doi: 10.1016/j.dsr.2011.08.002 94. Kraft, A. (2010): Amphipods observed in sediment trap samples in the eastern Fram Strait (Arctic [...] Somavilla, R. , Bauerfeind, E. and Beszczynska-Möller, A. (2015): Exchange of warming deep waters across Fram Strait , Deep-Sea Research Part I-Oceanographic Research Papers, 103 , pp. 86-100 . 2. Soltwedel,

flow over Fram Strait during cold-air outbreaks The model METRAS was applied to simulate different days of the aircraft campaign covering a domain of 320 x 450 km2 in the northern part of Fram Strait (Figure [...] Svalbard campaign The field observations were planned on the basis of earlier investigations in the Fram Strait region (Figure 1). Three different operations were conducted. First, ground based measurements [...] attempts were based on data of an aircraft campaign which was carried out in the environment of Svalbard (Fram Strait and Storefjord). The means for the model investigations are the three-dimensional non-hydrostatic

PS93.1 Weekly Report No. 1 | 29 June to 5 July 2015
At 8:00 am the embarkment of scientists starts. As Polarstern cannot enter the harbor pier directly, people have to use the Zodiac (Fig.1).

the marine habitats of the High North. This is indicated by data from long-term observations in the Fram Strait, which researchers from the Alfred Wegener Institute (AWI) have now analysed. Their most important

lead to study areas northwest of Bear Island, south of Spitsbergen and in the central and eastern Fram Strait.

week was characterized by intense station work both in the West Spitsbergen Current and in central Fram Strait.

oceanographic, biological and biogeochemical workload planned along the zonal transect through central Fram Strait along 78°50’N. Subsequently we added to the mooring array deployed along the Greenwich Meridian