Variability of the Arctic Frontal Zone Characteristics in the Barents and Kara Seas in the First Two Decades of the XXI Century
A. A. Konik1, 2, ✉, A. V. Zimin1, 2
1 P. P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Saint-Petersburg, Russian Federation
2 Saint Petersburg State University, Saint-Petersburg, Russian Federation
✉ e-mail: konikrshu@gmail.com
Abstract
Purpose. The article is devoted to studying the long-term variability of the characteristics of surface manifestations of the Arctic Frontal Zone formed seasonally in the Marginal Ice Zone of the Arctic seas.
Methods and Results. To identify the frontal zone, the satellite measurements of surface temperature carried out by the MODIS/Aqua and VIIRS/Suomi NPP from August to September 2002–2020 are used as initial data. The Arctic Frontal Zone position and characteristics were determined using the cluster analysis. In the warm period of the year, the average long-term thermal surface gradient in the Arctic Frontal Zone is revealed to be 0.06 °C/km, and its area – 348,000 km2. Variability of the interannual gradient estimates in this region ranged from 0.04 to 0.09 °C/km, and the area – from 159,000 to 489,000 km2.
Conclusions. During the last two decades, spatial position of the frontal zone has been characterized by a significant shift to the north (81°–82°N). The surface temperature in the frontal zone in the last decade was on average higher than that in the previous one. Such dynamics is conditioned by retreat of the arctic ice cover edge. The thermal gradient maximum values in the Arctic Frontal Zone were recorded in 2009, 2016 and 2018 at the significant near-surface wind speeds and the reduced ice cover concentration. The surface temperature, the thermal gradient and the frontal zone area are shown to be conditioned by the ice area and concentration in last year’s autumn season. It is established that during a warm season, the North Atlantic Oscillation winter index governs variation of the surface temperature in the Arctic Frontal Zone.
Keywords
Arctic zone, frontal zone, marginal ice zone, ice cover, satellite measurements, NAO, Barents Sea, Kara Sea
Acknowledgements
The study was carried out within the framework of the RFBR grant No. 20–35–90053 and state assignment of IO RAS on theme FMWE–2021–0014.
Original russian text
Original Russian Text © A. A. Konik, A. V. Zimin, 2022, published in MORSKOY GIDROFIZICHESKIY ZHURNAL, Vol. 38, Iss. 6, pp. 679-693 (2022)
For citation
Konik, A.A. and Zimin, A.V., 2022. Variability of the Arctic Frontal Zone Characteristics in the Barents and Kara Seas in the First Two Decades of the XXI Century. Physical Oceanography, 29(6), pp. 659-673. doi:10.22449/1573-160X-2022-6-659-673
DOI
10.22449/1573-160X-2022-6-659-673
References
- Kumar, A., Yadav, J. and Mohan, R., 2021. Spatio-Temporal Change and Variability of BarentsKara Sea Ice, in the Arctic: Ocean and Atmospheric Implications. Science of The Total Environment, 753, 142046. doi:10.1016/j.scitotenv.2020.142046
- Parkinson, C.L. and Cavalieri, D.J., 2008. Arctic Sea Ice Variability and Trends, 1979–2006. Journal of Geophysical Research: Oceans, 113(C7), C07003. doi:10.1029/2007jc004558
- Maslanik, J., Stroeve, J., Fowler, C. and Emery, W., 2011. Distribution and Trends in Arctic Sea Ice Age through Spring 2011. Geophysical Research Letters, 38(13), L13502. doi:10.1029/2011gl047735
- Serreze, M.C. and Stroeve, J., 2015. Arctic Sea Ice Trends, Variability and Implications for Seasonal Ice Forecasting. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 373(2045), 20140159. doi:10.1098/rsta.2014.0159
- Collins, C.O., Rogers, W.E., Marchenko, A. and Babanin, A.V., 2015. In Situ Measurements of an Energetic Wave Event in the Arctic Marginal Ice Zone. Geophysical Research Letters, 42(6), pp. 1863-1870. doi:10.1002/2015gl063063
- McPhee, M.G., Maykut, G.A. and Morison, J.H., 1987. Dynamics and Thermodynamics of the Ice/Upper Ocean System in the Marginal Ice Zone of the Greenland Sea. Journal of Geophysical Research: Oceans, 92(C7), pp. 7017-7031. doi:10.1029/jc092ic07p07017
- Ginsburg, A.I. and Fedorov, K.N., 1989. On the Multitude of Forms of Coherent Motions in Marginal ICE Zones (MIZ). In: J. C. J. Nihoul and B. M. Jamart, eds., 1989. Mesoscale/Synoptic Coherent Structures in Geophysical Turbulence. Elsevier Oceanography Series, vol. 50. Amsterdam: Elsevier B.V., pp. 25-39. doi:10.1016/s0422-9894(08)70175-2
- Ivanov, V.V., Alekseyev, V.A. and Repina, I.A., 2014. [The Increasing Impact of Atlantic Waters on the Ice Cover of the Arctic Ocean]. In: The International Conference dedicated to the memory of academician A. M. Obukhov “Turbulence, Atmosphere and Climate Dynamics”. 13-16 May 2013. Abstracts. Moscow, 13–16 May 2013. Moscow: GEOS, pp. 336-344 (in Russian).
- Selivanova, J.V., Tilinina, N.D., Gulev, S.K., and Dobrolubov, S.A. 2016. Impact of Ice Cover in the Arctic on Ocean-Atmosphere Turbulent Heat Fluxes. Oceanology, 56(1), pp. 14-18. doi:10.1134/S0001437016010185
- Kędra, M., Moritz, C., Choy, E.S., David, C., Degen, R., Duerksen, S., Ellingsen, I., Gorska, B., Grebmeier, J.M. [et al.], 2015. Status and Trends in the Structure of Arctic Benthic Food Webs. Polar Research, 34(1), 23775. doi:10.3402/polar.v34.23775
- Makarevich, P.R. and Oleinik, A.A., 2017. Barents Sea Phytoplankton during Springtime: Composition and Structure at the Sea Ice Edge. Transactions of the Kola Science Centre, 8(2-4), pp. 50-58. Available at: http://www.mmbi.info/fs/files/1290/Okeanologiia_vyp_4_trudy_2_17.pdf [Accessed: 04 April 2022] (in Russian).
- Van Aken, H.M., Budéus, G. and Hähnel, M., 1995. The Anatomy of the Arctic Frontal Zone in the Greenland Sea. Journal of Geophysical Research: Oceans, 100(C8), pp. 15999-16014. doi:10.1029/95jc01176
- Rodionov, V.B. and Kostianoy, A.G., 1998. Oceanic Fronts of the Seas of the NorthEuropean Basin Seas. Moscow: GEOS, 292 p. (in Russian).
- Konik, A.A., Zimin, A.V. and Atadzhanova, O.A., 2019. Quantitative Estimations of the Variability of Characteristics of the Temperature of the Sea Surface in the Front of the Frontal Zone of the Kara Sea. Fundamental and Applied Hydrophysics, 12(1), pp. 54-61. doi:10.7868/S2073667319010076 (in Russian).
- Brenner, S., Rainville, L., Thomson, J. and Lee, C., 2020. The Evolution of a Shallow Front in the Arctic Marginal Ice Zone. Elementa: Science of the Anthropocene, 8, 17. doi:10.1525/elementa.413
- Moiseev, D.V. and Zhichkin, A.P., 2017. Thermohaline Conditions of Ice Edge Area in the Northern Barents Sea in April 2016. Transactions of the Kola Science Centre, 8(2-4), pp. 10-25. Available at: http://www.mmbi.info/fs/files/1290/Okeanologiia_vyp_4_trudy_2_17.pdf [Accessed: 04 April 2022] (in Russian).
- Atadzhanova, O.A. and Zimin, A.V., 2019. Analysis of the Characteristics of the Submesoscale Eddy Manifestations in the Barents, the Kara and the White Seas Using Satellite Data. Fundamental and Applied Hydrophysics, 12(3), pp. 36-45. doi:10.7868/S2073667319030055
- Liu, Y. and Minnett, P.J., 2016. Sampling Errors in Satellite-Derived Infrared SeaSurface Temperatures. Part I: Global and Regional MODIS Fields. Remote Sensing of Environment, 177, pp. 48-64. doi:10.1016/j.rse.2016.02.026
- Ivshin, V.A., Trofimov, A.G. and Titov, O.V., 2019. Barents Sea Thermal Frontal Zones in 1960–2017: Variability, Weakening, Shifting. ICES Journal of Marine Science, 76(suppl. 1), pp. i3-i9. doi:10.1093/icesjms/fsz159
- Spreen, G., Kaleschke, L. and Heygster, G., 2008. Sea Ice Remote Sensing Using AMSR‐E 89-GHz Channels. Journal of Geophysical Research: Oceans, 113(C2), C02S03. doi:10.1029/2005JC003384
- Nesterov, E.S., 2013. North Atlantic Oscillation: Atmosphere and Ocean. Moscow: Triada Ltd., 144 p. (in Russian).
- Osadchiev, A.A., 2021. River Plumes. Moscow: Scientific World, 284 p. (in Russian).
- Johannessen, O.M. and Foster, L.A., 1978. A Note on the Topographically Controlled Oceanic Polar Front in the Barents Sea. Journal of Geophysical Research: Oceans, 83(C9), pp. 4567-4571. doi:10.1029/jc083ic09p04567
- Pavlov, V.K. and Pfirman, S.L., 1995. Hydrographic Structure and Variability of the Kara Sea: Implications for Pollutant Distribution. Deep Sea Research Part II: Topical Studies in Oceanography, 42(6), pp. 1369-1390. doi:10.1016/09670645(95)00046-1
- Harris, C.L., Plueddemann, A.J. and Gawarkiewicz, G.G., 1998. Water Mass Distribution and Polar Front Structure in the Western Barents Sea. Journal of Geophysical Research: Oceans, 103(C2), pp. 2905-2917. doi:10.1029/97jc02790
- Bauch, D. and Cherniavskaia, E., 2018. Water Mass Classification on a Highly Variable Arctic Shelf Region: Origin of Laptev Sea Water Masses and Implications for the Nutrient Budget. Journal of Geophysical Research: Oceans, 123(3), pp. 18961906. doi:10.1002/2017jc013524