Seasonal and Interannual Variations of Heat Fluxes in the Barents Sea Region

被引:7
作者
Bashmachnikov, I. L. [1 ,2 ]
Yurova, A. Yu [1 ,2 ]
Bobylev, L. P. [2 ,3 ]
Vesman, A. V. [2 ,4 ]
机构
[1] St Petersburg State Univ, St Petersburg 199034, Russia
[2] Nansen Int Environm & Remote Sensing Ctr, St Petersburg 199034, Russia
[3] Nansen Environm & Remote Sensing Ctr, N-5006 Bergen, Norway
[4] Arctic & Antarctic Res Inst, State Res Ctr, St Petersburg 199397, Russia
基金
俄罗斯科学基金会;
关键词
Barents Sea; MIT eddy-permitting ocean model; oceanic and atmospheric heat fluxes; coupled cycles in the ocean and the atmosphere; Bjerknes compensation mechanism; wavelet analysis; singular spectral analysis; OCEAN; VARIABILITY; TRANSPORT; CIRCULATION; CLIMATE;
D O I
10.1134/S0001433818020032
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Seasonal and interannual variations in adjective heat fluxes in the ocean (dQ(oc)) and the convergence of advective heat fluxes in the atmosphere (dQ(atm)) in the Barents Sea region have been investigated over the period of 1993-2012 using the results of the MIT regional eddy-permitting model and ERA-Interim atmospheric reanalysis. Wavelet analysis and singular spectrum analysis are used to reveal concealed periodicities. Seasonal 2- to 4- and 5- to 8-year cycles are revealed in the dQ(oc) and dQ(atm) data. It is also found that seasonal variations in dQ(oc) are primarily determined by the integrated volume fluxes through the western boundary of the Barents Sea, whereas the 20-year trend is determined by the temperature variation of the transported water. A cross-wavelet analysis of dQ(oc) and dQ(atm) in the Barents Sea region shows that the seasonal variations in dQ(oc) and dQ(atm) are nearly in-phase, while their interannual variations are out-of-phase. It is concluded that the basin of the Barents Sea plays an important role in maintaining the feedback mechanism (the Bjerknes compensation) of the ocean-atmosphere system in the Arctic region.
引用
收藏
页码:213 / 222
页数:10
相关论文
共 52 条
[1]  
Alekseev GV, 2001, IZV ATMOS OCEAN PHY+, V37, P341
[2]  
Antonov V. S., 1968, T AANII, V285, P148
[3]  
Astafieva N.M., 1996, Phys. Uspekhi, V39, P1085, DOI DOI 10.1070/PU1996V039N11ABEH000177
[4]   Intra-annual and interannual non-stationary cycles of chlorophyll concentration in the Northeast Atlantic [J].
Bashmachnikov, I. ;
Belonenko, T. V. ;
Koldunov, A. V. .
REMOTE SENSING OF ENVIRONMENT, 2013, 137 :55-68
[5]  
Bengtsson L, 2004, J CLIMATE, V17, P4045, DOI 10.1175/1520-0442(2004)017<4045:TETWIT>2.0.CO
[6]  
2
[7]  
Bjerknes J., 1964, ADV GEOPHYS, V10, P1, DOI [10.1016/S0065-2687(08)60005-9, DOI 10.1016/S0065-2687(08)60005-9]
[8]  
Blindheim J., 1989, Rapp. P.V. Reun. Cons. Int. Explor. Mer, V188, P49
[9]  
Clement Kinney J., 2014, The Pacific Arctic Region, P167, DOI [10.1007/978-94-017-8863-27, DOI 10.1007/978-94-017-8863-27]
[10]   The ERA-Interim reanalysis: configuration and performance of the data assimilation system [J].
Dee, D. P. ;
Uppala, S. M. ;
Simmons, A. J. ;
Berrisford, P. ;
Poli, P. ;
Kobayashi, S. ;
Andrae, U. ;
Balmaseda, M. A. ;
Balsamo, G. ;
Bauer, P. ;
Bechtold, P. ;
Beljaars, A. C. M. ;
van de Berg, L. ;
Bidlot, J. ;
Bormann, N. ;
Delsol, C. ;
Dragani, R. ;
Fuentes, M. ;
Geer, A. J. ;
Haimberger, L. ;
Healy, S. B. ;
Hersbach, H. ;
Holm, E. V. ;
Isaksen, L. ;
Kallberg, P. ;
Koehler, M. ;
Matricardi, M. ;
McNally, A. P. ;
Monge-Sanz, B. M. ;
Morcrette, J. -J. ;
Park, B. -K. ;
Peubey, C. ;
de Rosnay, P. ;
Tavolato, C. ;
Thepaut, J. -N. ;
Vitart, F. .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2011, 137 (656) :553-597