Abstract
Sensitivity study of the air–ice drag coefficient C Dai is presented with an ice–ocean coupled model for the Sea of Okhotsk. The C Dai × 103 value is varied from 2 to 5 based on the direct measurements in the region. The maximum volume transport of the East Sakhalin Current and the mean sea ice velocity were intensified as C Dai increased. The sensitivity experiment with the ice–water drag coefficient C Diw showed that the East Sakhalin Current volume transport is hardly affected by C Diw but significantly intensified by C Dai. While the ice drift in the off-ice-edge direction was intensified by the increase in C Dai and the decrease in C Diw, the ice edge location was nearly unchanged. This was due to melting caused by the relatively warm water inflow from the North Pacific. That is, sea ice extent in the region is strongly influenced by melting caused by a large ice–ocean heat transfer. In the active melting regions, the ice–ocean heat transfer of more than 100 W/m2 occurred even in mid-winter. This is the same order as the cooling by air in winter, and a heat insulation capacity of sea ice is weakened in such regions.
Similar content being viewed by others
References
Fujisaki A, Yamaguchi H, Toyota T, Futatsudera A, Miyanaga M (2009) Measurements of air–ice drag coefficient over the ice-covered Sea of Okhotsk. J Oceanogr 65:487–498
Gladyshev S, Talley L, Kantakov G, Khen G, Wakatsuchi M (2003) Distribution, formation, and seasonal variability of Okhotsk Sea Mode Water. J Geophys Res 108(C6):3186. doi:10.1029/2001JC000877
Guest PS, Davidson KL (1991) The aerodynamic roughness of different types of sea ice. J Geophys Res 96(C3):4709–4721. doi:10.1029/90JC02261
Hibler WD (1979) Dynamic thermodynamics sea ice model. J Phys Oceanogr 9:815–846. doi:10.1175/1520-0485(1979)009<0815:ADTSIM>2.0.CO;2
Hunke EC, Duckowicz JK (1997) An elastic-viscous-plastic model for sea ice dynamics. J Phys Oceanogr 27:1849–1867. doi:10.1175/1520-0485(1997)027<1849:AEVPMF>2.0.CO;2
Itoh M, Ohshima KI, Wakatsuchi M (2003) Distribution and formation of Okhotsk Sea intermediate water: an analysis of isopycnal climatological data. J Geophys Res 108(C8):14. doi:10.1029/2002JC001590
Lapko VV, Radchenko VI (2000) Sea of Okhotsk. Mar Pollut Bull 41(1–6):179–187. doi:10.1016/S0025-326X(00)00109-0
Large WG, Pond S (1981) Open ocean momentum flux measurements in moderate to strong winds. J Phys Oceanogr 11(3):324–336. doi:10.1175/1520-0485(1981)011<0324:OOMFMI>2.0.CO;2
Leppäranta M (2005) The drift of sea ice. Springer, Berlin
Levitus, S, Burgett R, Boyer TP (1994) Salinity. World Ocean Atlas 1994. NOAA Atlas NESDIS. 3(99)
Matsuda J, Mitsudera H, Nakamura T, Uchimoto K, Nakanowatari T, Ebuchi N (2009) Wind and buoyancy driven intermediate-layer overturning in the Sea of Okhotsk. Deep-Sea Res 56:1401–1418
McPhee MG, Kottmeier C, Morrison JH (1998) Ocean heat flux in the Central Weddell Sea during winter. J Phys Oceanogr 29(6):1166–1179. doi:10.1175/1520-0485(1999)029<1166:OHFITC>2.0.CO;2
McPhee MG, Morison JH, Nilsen F (2008) Revisiting heat and salt exchange at the ice–ocean interface: ocean flux and modeling considerations. J Geophys Res 113(C06014). doi:10.1029/2007JC004383
Mizuta G, Fukamachi Y, Ohshima KI (2003) Structure and seasonal variability of the East Sakhalin Current. J Phys Oceanogr 33(11):2430–2445. doi:10.1175/1520-0485(2003)033<2430:SASVOT>2.0.CO;2
Nakamura T, Awaji T (2004) Tidally induced diapycnal mixing in the Kuril Straits and its role in water transformation and transport. J Geophys Res 109(C09S07). doi:10.1029/2003JC001850
Nakamura T, Toyoda T, Ishikawa Y, Awaji T (2006) Effects of tidal mixing at the Kuril Straits on the North Pacific ventilation: Adjustment of intermediate layer revealed from numerical experiments. J Geophys Res 111(C04003). doi:10.1029/2005JC003142
Nakanowatari T, Ohshima KI, Wakatsuchi M (2007) Warming and oxygen decrease of intermediate water in the northwestern North Pacific, originating from the Sea of Okhotsk, 1955–2004. Geophys Res Lett 34(L04602). doi:10.1029/2006GL028243
Nishioka J, Ono T, Saito H, Nakatsuka T, Takeda S, Yoshimura T, Suzuki K, Kuma K, Nakabayashi S, Tsumune D, Mitsudera H, Johnsin WK, Tsuda A (2007) Iron supply to the western subarctic Pacific: Importance of iron export from the Sea of Okhotsk. J Geophys Res 112(C10012). doi:10.1029/2006JC004055
Ohshima KI, Wakatsuchi M, Fukamachi Y (2002) Near-surface circulation and tidal currents of the Okhotsk Sea observed with satellite-tracked drifters. J Geophys Res 107(C11):C16
Ohshima KI, Watanabe T, Nihashi S (2003) Surface Heat Budget of the Sea of Okhotsk during 1987–2001 and the role of sea ice on it. J Meteorol Soc Jpn 81(4):653–677
Ohshima KI, Simizu D, Itoh M, Fukamachi Y, Wakatsuchi S (2004) Sverdrup balance and the cyclonic gyre in the Sea of Okhotsk. J Phys Oceanogr 34(2):513–525. doi:10.1175/1520-0485(2004)034<0513:SBATCG>2.0.CO;2
Parkinson CL, Washington WM (1979) A large-scale numerical model 789 of sea ice. J Geophys Res 84(C1):311–337
Perovich DK, Elder B (2002) Estimates of ocean heat flux at SHEBA. Geophys Res Lett 29(9):58
Sagawa G (2007) Development of ice dynamic model that takes account of floe collision and its validation in numerical sea ice forecast in the Sea of Okhotsk, Dissertation, University of Tokyo
Semtner AJ (1979) A model for the thermodynamic growth of sea ice in numerical investigations of climate. J Phys Oceanogr 6(3):379–389
Shcherbina AY, Talley LD, Rudnick DL (2004a) Dense water formation on the northwestern shelf of the Okhotsk Sea: 1. Direct observations of brine rejection. J Geophys Res 109(C09S08). doi:10.1029/2003JC002196
Shcherbina AY, Talley LD, Rudnick DL (2004b) Dense water formation on the northwestern shelf of the Okhotsk Sea: 2. Quantifying the transports. J Geophys Res 109(C09S09). doi:10.1029/2003JC002197
Shen H, Hibler W, Leppäranta M (1987) The role of floe collisions in sea ice rheology. J Geophys Res 92(C7):7085–7096
Shirasawa K (1981) Studies on wind stress on sea ice. Low Temp Sci Ser A 40:101–118
Simizu D, Ohshima KI (2006) A model simulation on the circulation in the Sea of Okhotsk and the East Sakhalin Current. J Geophys Res 111(C05016). doi:10.1029/2005JC002980
Tang CL, Detracy BM (1998) Space-time variation of mixed layer properties, heat and salt fluxes, and ice melt in the Newfoundland marginal ice zone. J Geophys Res 103(C1):1177–1191
Toyota T, Kawamura T, Ohshima KI, Shimoda H, Wakatsuchi M (2004) Thickness distribution, texture and stratigraphy, and a simple probabilistic model for dynamical thickening of sea ice in the southern Sea of Okhotsk. J Geophys Res 109(C06001). doi:10.1029/2003JC002090
Uchimoto K, Mitsudera H, Ebuchi N, Miyazawa Y (2007) Anticyclonic eddy caused by the Soya Warm Current in an Okhotsk OGCM. J Oceanogr 63:379–391
Acknowledgments
The authors wish to thank the sea ice group of office of marine prediction, the Japan Meteorological Agency who provided the sea ice analysis, and the objective analysis by the Regional Spectral Value. We also thank the group of Prof. K.I. Ohshima in the Institute of Low Temperature Science, Hokkaido University, who provided the merged observation data of the sea surface salinity.
Author information
Authors and Affiliations
Corresponding author
Additional information
Responsible Editor: Leo Oey
Rights and permissions
About this article
Cite this article
Fujisaki, A., Yamaguchi, H. & Mitsudera, H. Numerical experiments of air–ice drag coefficient and its impact on ice–ocean coupled system in the Sea of Okhotsk. Ocean Dynamics 60, 377–394 (2010). https://doi.org/10.1007/s10236-010-0265-7
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10236-010-0265-7