Submesoscale processes in the Baltic Sea
Chrysagi, Evridiki
1984-
VerfasserIn
aut
Burchard, Hans
1959-
AkademischeR BetreuerIn
dgs
Elken, Jüri
AkademischeR BetreuerIn
dgs
Universität Rostock
Grad-verleihende Institution
dgg
Universität Rostock
Mathematisch-Naturwissenschaftliche Fakultät
Grad-verleihende Institution
dgg
text
theses
Text
Hochschulschrift
gw
2020
monographic
XA-DE
Rostock
Universität
publisher
2020
Rostock
Universitätsbibliothek
distributor
eng
1 Online-Ressource
Recently discovered, ocean submesoscales have attracted attention due to their ability to change the upper ocean stratification and induce a downscale cascade of energy. Those motions have been studied mainly in the context of open ocean simulations and idealized configurations; however, their response during cooling and strong winds, is still unclear. Here, realistic simulations of the central Baltic Sea revealed not only that submesoscales are abundant in the basin but also that they are able to maintain shallow mixed layers during storms and quickly restratify between multiple wind events.<eng>
vorgelegt von Evridiki Chrysagi
Zeitschriftenpublikation: Chrysagi, E., Umlauf, L., Holtermann, P., Klingbeil, K., & Burchard, H. (2021). High‐resolution simulations of submesoscale processes in the Baltic Sea: The role of storm events. Journal of Geophysical Research: Oceans, 126, e2020JC016411. https://doi.org/10.1029/2020JC016411
GutachterInnen: Hans Burchard (Leibniz-Institut für Ostseeforschung Warnemünde) ; Jüri Elken (Tallinn University of Technology)
Dissertation Universität Rostock 2021
333.7
530
550
551.462
550
UT 5600
38.90
http://purl.uni-rostock.de/rosdok/id00002961
https://doi.org/10.18453/rosdok_id00002961
https://nbn-resolving.org/urn:nbn:de:gbv:28-rosdok_id00002961-5
https://d-nb.info/1293662666/34
Submesoscale processes in the Baltic Sea
Rostock, 2020
Druck-Ausgabe
(DE-627)1750552272
Chrysagi, Evridiki, 1984 -
urn:nbn:de:gbv:28-rosdok_id00002961-5
10.18453/rosdok_id00002961
1240158772
rda
DE-627
210301
1750038250
20251226T192359.0
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