Zobrazeno 1 - 10
of 306
pro vyhledávání: '"U. Schauer"'
Publikováno v:
Earth System Science Data, Vol 11, Pp 895-920 (2019)
During summer 2014 and summer 2015 two autonomous Seagliders were operated over several months close to the ice edge of the East Greenland Current to capture the near-surface freshwater distribution in the western Greenland Sea. The mission in 2015 i
Externí odkaz:
https://doaj.org/article/610b6331eafe4ebcbd96b0a80db55b3e
Publikováno v:
Earth System Science Data, Vol 10, Pp 1119-1138 (2018)
UDASH (Unified Database for Arctic and Subarctic Hydrography) is a unified and high-quality temperature and salinity data set for the Arctic Ocean and the subpolar seas north of 65° N for the period 1980–2015. The archive aims at including all p
Externí odkaz:
https://doaj.org/article/2536304f1cbf4de292c72f5b952638cc
Autor:
H. Sumata, F. Kauker, M. Karcher, B. Rabe, M.-L. Timmermans, A. Behrendt, R. Gerdes, U. Schauer, K. Shimada, K.-H. Cho, T. Kikuchi
Publikováno v:
Ocean Science, Vol 14, Pp 161-185 (2018)
Any use of observational data for data assimilation requires adequate information of their representativeness in space and time. This is particularly important for sparse, non-synoptic data, which comprise the bulk of oceanic in situ observations
Externí odkaz:
https://doaj.org/article/625a1a5df6854448aabfc9dbe6b3efb0
Autor:
I. A. Dmitrenko, S. A. Kirillov, N. Serra, N. V. Koldunov, V. V. Ivanov, U. Schauer, I. V. Polyakov, D. Barber, M. Janout, V. S. Lien, M. Makhotin, Y. Aksenov
Publikováno v:
Ocean Science, Vol 10, Iss 4, Pp 719-730 (2014)
A distinct, subsurface density front along the eastern St. Anna Trough in the northern Kara Sea is inferred from hydrographic observations in 1996 and 2008–2010. Direct velocity measurements show a persistent northward subsurface current (~ 18 cm s
Externí odkaz:
https://doaj.org/article/77f217797f91471f8fc36b08e2976b61
Publikováno v:
Ocean Science, Vol 9, Iss 1, Pp 147-169 (2013)
The circulation and water mass properties in the Eurasian Basin are discussed based on a review of previous research and an examination of observations made in recent years within, or parallel to, DAMOCLES (Developing Arctic Modeling and Observationa
Externí odkaz:
https://doaj.org/article/3500df684a2c40fe86d025de8862a2c3
Autor:
G. Kattner, A. Beszczynska-Möller, A. Mackensen, U. Schauer, E. Hansen, E. Falck, P. A. Dodd, B. Rabe, E. J. Rohling, K. Cox
Publikováno v:
Ocean Science, Vol 9, Iss 1, Pp 91-109 (2013)
We estimated the magnitude and composition of southward liquid freshwater transports in the East Greenland Current near 79° N in the Western Fram Strait between 1998 and 2011. Previous studies have found this region to be an important pathway for li
Externí odkaz:
https://doaj.org/article/89c60dbb78754617856f8d7bbe51cce5
Publikováno v:
Biogeosciences, Vol 7, Iss 3, Pp 1099-1108 (2010)
A methane surplus relative to the atmospheric equilibrium is a frequently observed feature of ocean surface water. Despite the common fact that biological processes are responsible for its origin, the formation of methane in aerobic surface water is
Externí odkaz:
https://doaj.org/article/9b0a996473a44e5f8fccc196872b5f60
Autor:
U. Schauer, A. Beszczynska-Möller
Publikováno v:
Ocean Science, Vol 5, Iss 4, Pp 487-494 (2009)
While the concept of oceanic heat transport – or rather heat transport divergence – is well known, it is sometimes applied inaccurately. Often so-called "heat transports" are computed across a partial section which means that the volume flow thro
Externí odkaz:
https://doaj.org/article/b51ff5b59c5c435b84fa5be1669bd9db
Publikováno v:
Ocean Science, Vol 5, Iss 3, Pp 219-233 (2009)
We present the late summer distribution and transports of freshwater components in the upper western part of the Fram Strait during 1998, 2004 and 2005. Hydrographic data and and water δ18O values are analyzed to distinguish Atlantic Water, ice melt
Externí odkaz:
https://doaj.org/article/d6501a41970f41e2911b0f7afcd143e2
Autor:
U. Schauer, B. Rudels, E. P. Jones, L. G. Anderson, R. D. Muench, G. Björk, J. H. Swift, V. Ivanov, A.-M. Larsson
Publikováno v:
Annales Geophysicae, Vol 20, Pp 257-273 (2002)
The waters in the Eurasian Basin are conditioned by the confluence of the boundary flow of warm, saline Fram Strait water and cold low salinity water from the Barents Sea entering through the St. Anna Trough. Hydrographic sections obtained from
Externí odkaz:
https://doaj.org/article/77c2eea38ed74e0c8540371d4db2687a