Articles | Volume 14, issue 2
The Cryosphere, 14, 477–495, 2020
https://doi.org/10.5194/tc-14-477-2020
The Cryosphere, 14, 477–495, 2020
https://doi.org/10.5194/tc-14-477-2020

Research article 05 Feb 2020

Research article | 05 Feb 2020

Sea ice volume variability and water temperature in the Greenland Sea

Valeria Selyuzhenok et al.

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Cited articles

Alekseev, G., Johannessen, O., and Kovalevskii, D.: Development of convective motions under the effect of local perturbations of sea-surface density, Izv. Atmos. Ocean. Phy., 37, 341–350, 2001. a
Alekseev, G. V., V., B. P., and Nagurnij, A.: Struktura termokhalinnikn polej v rajone tsiklonicheskoj tsirkulatsii i podnyatiya vod, in: Struktura i izmenchivist' krupnomasshtabnyh okeanologicheskih processov i polej v Norvezhskoj energoaktivnoj zone, Gidrometizdat, Leningrad, 18–27, 1989 (in Russian). a
Alekseev, G. V., Johannessen, O., and Kovalevsky, D. V.: On development of convective motions under the influence of local density perturbations on the sea surface, Atmos. Ocean Phys., 37, 368–377, 2001a. a
Alekseev, G. V., Johannessen, O. M., Korablev, A. A., Ivanov, V. V., and Kovalevsky, D. V.: Interannual variability in water masses in the Greenland Sea and adjacent areas, Polar Res., 20, 201–208, https://doi.org/10.1038/ncomms2505, 2001b. a
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This study explores a link between the long-term variations in the integral sea ice volume in the Greenland Sea and oceanic processes. We link the changes in the Pan-Arctic Ice Ocean Modeling and Assimilation System (PIOMAS) regional sea ice volume with the mixed layer, depth and upper-ocean heat content derived using the ARMOR dataset.