Volume 41 Issue 7
Jul.  2022
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Xiaomin Chang, Longchun Ye, Guangyu Zuo, Jingyue Li, Keyu Wei, Yinke Dou. Characteristics of sea ice kinematics from the marginal ice zone to the packed ice zone observed by buoys deployed during the 9th Chinese Arctic Expedition[J]. Acta Oceanologica Sinica, 2022, 41(7): 113-127. doi: 10.1007/s13131-022-1990-8
Citation: Xiaomin Chang, Longchun Ye, Guangyu Zuo, Jingyue Li, Keyu Wei, Yinke Dou. Characteristics of sea ice kinematics from the marginal ice zone to the packed ice zone observed by buoys deployed during the 9th Chinese Arctic Expedition[J]. Acta Oceanologica Sinica, 2022, 41(7): 113-127. doi: 10.1007/s13131-022-1990-8

Characteristics of sea ice kinematics from the marginal ice zone to the packed ice zone observed by buoys deployed during the 9th Chinese Arctic Expedition

doi: 10.1007/s13131-022-1990-8
Funds:  The National Key Research and Development Program of China under contract No. 2016YFC1402702; the Basic Research Program of Shanxi Province under contract No. 202103021224054.
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  • Corresponding author: E-mail: changxiaomin@tyut.edu.cn
  • Received Date: 2021-09-17
  • Accepted Date: 2021-11-09
  • Available Online: 2022-04-07
  • Publish Date: 2022-07-08
  • Sea ice growth and consolidation play a significant role in heat and momentum exchange between the atmosphere and the ocean. However, few in situ observations of sea ice kinematics have been reported owing to difficulties of deployment of buoys in the marginal ice zone (MIZ). To investigate the characteristics of sea ice kinematics from MIZ to packed ice zone (PIZ), eight drifting buoys designed by Taiyuan University of Technology were deployed in the open water at the ice edge of the Canadian Basin. Sea ice near the buoy constantly increased as the buoy drifted, and the kinematics of the buoy changed as the buoy was frozen into the ice. This process can be determined using sea ice concentration, sea skin temperature, and drift speed of buoy together. Sea ice concentration data showed that buoys entered the PIZ in mid-October as the ice grew and consolidated around the buoys, with high amplitude, high frequency buoy motions almost ceasing. Our results confirmed that good correlation coefficient in monthly scale between buoy drift and the wind only happened in the ice zone. The correlation coefficient between buoys and wind was below 0.3 while the buoys were in open water. As buoys entered the ice zone, the buoy speed was normally distributed at wind speeds above 6 m/s. The buoy drifted mainly to the right of the wind within 45° at wind speeds above 8 m/s. During further consolidation of the ice in MIZ, the direct forcing on the ice through winds will be lessened. The correlation coefficient value increased to 0.9 in November, and gradually decreased to 0.7 in April.
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  • [1]
    Aksenov Y, Popova E E, Yool A, et al. 2017. On the future navigability of Arctic sea routes: High-resolution projections of the Arctic Ocean and sea ice. Marine Policy, 75: 300–317. doi: 10.1016/j.marpol.2015.12.027
    [2]
    Alam A, Curry J A. 1998. Evolution of new ice and turbulent fluxes over freezing winter leads. Journal of Geophysical Research: Oceans, 103(C8): 15783–15802. doi: 10.1029/98JC01188
    [3]
    Assmy P, Fernández-Méndez M, Duarte P, et al. 2017. Leads in Arctic pack ice enable early phytoplankton blooms below snow-covered sea ice. Scientific Reports, 7(1): 40850. doi: 10.1038/srep40850
    [4]
    Aulicino G, Wadhams P, Parmiggiani F. 2019. SAR pancake ice thickness retrieval in the terra nova bay (Antarctica) during the PIPERS expedition in winter 2017. Remote Sensing, 11(21): 2510. doi: 10.3390/rs11212510
    [5]
    Beitsch A, Kaleschke L, Kern S. 2014. Investigating high-resolution AMSR2 sea ice concentrations during the February 2013 fracture event in the Beaufort Sea. Remote Sensing, 6(5): 3841–3856. doi: 10.3390/rs6053841
    [6]
    Boutin G, Lique C, Ardhuin F, et al. 2020. Towards a coupled model to investigate wave–sea ice interactions in the Arctic marginal ice zone. The Cryosphere, 14(2): 709–735. doi: 10.5194/tc-14-709-2020
    [7]
    Clem K R, Fogt R L, Turner J, et al. 2020. Record warming at the South Pole during the past three decades. Nature Climate Change, 10(8): 762–770. doi: 10.1038/s41558-020-0815-z
    [8]
    Delhasse A, Kittel C, Amory C, et al. 2020. Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet. The Cryosphere, 14(3): 957–965. doi: 10.5194/tc-14-957-2020
    [9]
    Doble M J. 2009. Simulating pancake and frazil ice growth in the Weddell Sea: A process model from freezing to consolidation. Journal of Geophysical Research: Oceans, 114(C9): C09003
    [10]
    Doble M J, Wadhams P. 2006. Dynamical contrasts between pancake and pack ice, investigated with a drifting buoy array. Journal of Geophysical Research: Oceans, 111(C11): C11S24
    [11]
    Gentemann C L, Scott J P, Mazzini P L F, et al. 2020. Saildrone: Adaptively sampling the marine environment. Bulletin of the American Meteorological Society, 101(6): E744–E762. doi: 10.1175/BAMS-D-19-0015.1
    [12]
    Gimbert F, Jourdain N C, Marsan D, et al. 2012a. Recent mechanical weakening of the Arctic sea ice cover as revealed from larger inertial oscillations. Journal of Geophysical Research: Oceans, 117(C11): C00J12
    [13]
    Gimbert F, Marsan D, Weiss J, et al. 2012b. Sea ice inertial oscillations in the Arctic Basin. The Cryosphere, 6(5): 1187–1201. doi: 10.5194/tc-6-1187-2012
    [14]
    Griebel J. 2020. Improvements and analyzes of sea ice drift and deformation retrievals from SAR images [dissertation]. Bremen: University of Bremen
    [15]
    Haller M, Brümmer B, Müller G. 2014. Atmosphere–ice forcing in the transpolar drift stream: results from the DAMOCLES ice-buoy campaigns 2007–2009. The Cryosphere, 8(1): 275–288. doi: 10.5194/tc-8-275-2014
    [16]
    Heil P, Hutchings J K, Worby A P, et al. 2008. Tidal forcing on sea-ice drift and deformation in the western Weddell Sea in early austral summer, 2004. Deep-Sea Research Part II: Topical Studies in Oceanography, 55(8–9): 943–962. doi: 10.1016/j.dsr2.2007.12.026
    [17]
    Horvat C, Tziperman E. 2017. The evolution of scaling laws in the sea ice floe size distribution. Journal of Geophysical Research: Oceans, 122(9): 7630–7650. doi: 10.1002/2016JC012573
    [18]
    Howell S E L, Tivy A, Yackel J J, et al. 2008. Changing sea ice melt parameters in the Canadian Arctic Archipelago: Implications for the future presence of multiyear ice. Journal of Geophysical Research: Oceans, 113(C9): C09030
    [19]
    Hutchings J K, Hibler W D III. 2008. Small-scale sea ice deformation in the Beaufort Sea seasonal ice zone. Journal of Geophysical Research: Oceans, 113(C8): C08032
    [20]
    Itkin P, Spreen G, Hvidegaard S M, et al. 2018. Contribution of deformation to sea ice mass balance: A case study from an N-ICE2015 storm. Geophysical Research Letters, 45(2): 789–796. doi: 10.1002/2017GL076056
    [21]
    Lee C M, Thomson J, The Marginal Ice Zone Team, et al. 2017. An autonomous approach to observing the seasonal ice zone in the western Arctic. Oceanography, 30(2): 56–68. doi: 10.5670/oceanog.2017.222
    [22]
    Lei Ruibo, Gui Dawei, Yuan Zhouli, et al. 2020. Characterization of the unprecedented polynya events north of Greenland in 2017/2018 using remote sensing and reanalysis data. Acta Oceanologica Sinica, 39(9): 5–17. doi: 10.1007/s13131-020-1643-8
    [23]
    Lei Ruibo, Heil P, Wang Jia, et al. 2016. Characterization of sea-ice kinematic in the Arctic outflow region using buoy data. Polar Research, 35(1): 22658. doi: 10.3402/polar.v35.22658
    [24]
    Lei Ruibo, Hoppmann M, Cheng Bin, et al. 2021. Seasonal changes in sea ice kinematics and deformation in the Pacific sector of the Arctic Ocean in 2018/19. The Cryosphere, 15(3): 1321–1341. doi: 10.5194/tc-15-1321-2021
    [25]
    Leppäranta M. 2011. The Drift of Sea Ice. 2nd ed. Berlin: Springer, 51–56
    [26]
    Liu Yue, Pang Xiaoping, Zhao Xi, et al. 2021. Prediction of the Antarctic marginal ICE zone extent based upon its multifractal property. Fractals, 29(2): 2150035. doi: 10.1142/S0218348X21500353
    [27]
    Lund B, Graber H C, Persson P O G, et al. 2018. Arctic sea ice drift measured by shipboard marine radar. Journal of Geophysical Research: Oceans, 123(6): 4298–4321. doi: 10.1029/2018JC013769
    [28]
    Lüpkes C, Vihma T, Birnbaum G, et al. 2008. Influence of leads in sea ice on the temperature of the atmospheric boundary layer during polar night. Geophysical Research Letters, 35(3): L03805
    [29]
    Manda A, Takahashi T, Komori S, et al. 2002. Validation of a new type of Lagrangian drifter using a GPS cellular phone. International Journal of Offshore and Polar Engineering, 12(3): 213–216
    [30]
    Moore G W K, Schweiger A, Zhang J, et al. 2018. Collapse of the 2017 winter Beaufort High: A response to thinning sea ice?. Geophysical Research Letters, 45(6): 2860–2869. doi: 10.1002/2017GL076446
    [31]
    Nansen F. 1902. Oceanography of the North Polar basin: the Norwegian North Polar Expedition 1893–96. Scientific Results, 3(9): 427
    [32]
    Notz D, Community S. 2020. Arctic sea ice in CMIP6. Geophysical Research Letters, 47(10): e2019GL086749
    [33]
    Qu Meng, Pang Xiaoping, Zhao Xi, et al. 2021. Spring leads in the Beaufort Sea and its interannual trend using Terra/MODIS thermal imagery. Remote Sensing of Environment, 256: 112342. doi: 10.1016/j.rse.2021.112342
    [34]
    Rampal P, Weiss J, Marsan D. 2009. Positive trend in the mean speed and deformation rate of Arctic sea ice, 1979–2007. Journal of Geophysical Research: Oceans, 114(C5)
    [35]
    Roach L A, Horvat C, Dean S M, et al. 2018a. An emergent sea ice floe size distribution in a global coupled ocean-sea ice model. Journal of Geophysical Research: Oceans, 123(6): 4322–4337. doi: 10.1029/2017JC013692
    [36]
    Roach L A, Smith M M, Dean S M. 2018b. Quantifying growth of pancake sea ice floes using images from drifting buoys. Journal of Geophysical Research: Oceans, 123(4): 2851–2866. doi: 10.1002/2017JC013693
    [37]
    Screen J A, Bracegirdle T J, Simmonds I. 2018. Polar climate change as manifest in atmospheric circulation. Current Climate Change Reports, 4(4): 383–395. doi: 10.1007/s40641-018-0111-4
    [38]
    Serreze M C, Barrett A P. 2011. Characteristics of the Beaufort Sea high. Journal of Climate, 24(1): 159–182. doi: 10.1175/2010JCLI3636.1
    [39]
    Shen H H, Ackley S F. 1991. A one-dimensional model for wave-induced ice-floe collisions. Annals of Glaciology, 15: 87–95. doi: 10.3189/1991AoG15-1-87-95
    [40]
    Shu Qi, Ma Hongyu, Qiao Fangli. 2012. Observation and simulation of a floe drift near the North Pole. Ocean Dynamics, 62(8): 1195–1200. doi: 10.1007/s10236-012-0554-4
    [41]
    Spreen G, Kaleschke L, Heygster G. 2008. Sea ice remote sensing using AMSR-E 89-GHz channels. Journal of Geophysical Research: Oceans, 113(C2): C02S03
    [42]
    Stroeve J C, Kattsov V, Barrett A, et al. 2012. Trends in Arctic sea ice extent from CMIP5, CMIP3 and observations. Geophysical Research Letters, 39(16)
    [43]
    Strong C, Foster D, Cherkaev E, et al. 2017. On the definition of marginal ice zone width. Journal of Atmospheric and Oceanic Technology, 34(7): 1565–1584. doi: 10.1175/JTECH-D-16-0171.1
    [44]
    Strong C, Rigor I G. 2013. Arctic marginal ice zone trending wider in summer and narrower in winter. Geophysical Research Letters, 40(18): 4864–4868. doi: 10.1002/grl.50928
    [45]
    Taylor M H, Losch M, Bracher A. 2013. On the drivers of phytoplankton blooms in the Antarctic marginal ice zone: A modeling approach. Journal of Geophysical Research: Oceans, 118(1): 63–75. doi: 10.1029/2012JC008418
    [46]
    Timmermans M L, Marshall J. 2020. Understanding Arctic Ocean circulation: a review of ocean dynamics in a changing climate. Journal of Geophysical Research: Oceans, 125(4): e2018JC014378
    [47]
    Uotila J, Vihma T, Launiainen J. 2000. Response of the Weddell Sea pack ice to wind forcing. Journal of Geophysical Research: Oceans, 105(C1): 1135–1151. doi: 10.1029/1999JC900265
    [48]
    Vichi M, Eayrs C, Alberello A, et al. 2019. Effects of an explosive polar cyclone crossing the Antarctic marginal ice zone. Geophysical Research Letters, 46(11): 5948–5958. doi: 10.1029/2019GL082457
    [49]
    Vihma T, Tisler P, Uotila P. 2012. Atmospheric forcing on the drift of Arctic sea ice in 1989–2009. Geophysical Research Letters, 39(2): L02501
    [50]
    Vinje T. 2001. Anomalies and trends of sea-ice extent and atmospheric circulation in the Nordic Seas during the period 1864–1998. Journal of Climate, 14(3): 255–267. doi: 10.1175/1520-0442(2001)014<0255:AATOSI>2.0.CO;2
    [51]
    Wang Jia, Zhang Jinlun, Watanabe E, et al. 2009. Is the Dipole Anomaly a major driver to record lows in Arctic summer sea ice extent?. Geophysical Research Letters, 36(5): L05706
    [52]
    Weeks W F, Ackley S F. 1986. The growth, structure, and properties of sea ice. In: Untersteiner N, ed. The Geophysics of Sea Ice. NATO ASI Series (Series B: Physics). Boston: Springer, 9–164
    [53]
    Willmes S, Heinemann G. 2016. Sea-ice wintertime lead frequencies and regional characteristics in the Arctic, 2003–2015. Remote Sensing, 8(1): 4
    [54]
    Wright N C, Polashenski C M. 2018. Open-source algorithm for detecting sea ice surface features in high-resolution optical imagery. The Cryosphere, 12(4): 1307–1329. doi: 10.5194/tc-12-1307-2018
    [55]
    Wu Bingyi. 2017. Winter atmospheric circulation anomaly associated with recent Arctic winter warm anomalies. Journal of Climate, 30(21): 8469–8479. doi: 10.1175/JCLI-D-17-0175.1
    [56]
    Wu Bingyi, Wang Jia, Walsh J E. 2006. Dipole anomaly in the winter Arctic atmosphere and its association with sea ice motion. Journal of Climate, 19(2): 210–225. doi: 10.1175/JCLI3619.1
    [57]
    Yang H, Choi J K, Park Y J, et al. 2014. Application of the Geostationary Ocean Color Imager (GOCI) to estimates of ocean surface currents. Journal of Geophysical Research: Oceans, 119(6): 3988–4000. doi: 10.1002/2014JC009981
    [58]
    Yu Yining, Xiao Wanxin, Zhang Zhilun, et al. 2021. Evaluation of 2-m air temperature and surface temperature from ERA5 and ERA-I using buoy observations in the Arctic during 2010–2020. Remote Sensing, 13(14): 2813. doi: 10.3390/rs13142813
    [59]
    Zhang Jinlun, Lindsay R, Schweiger A, et al. 2012. Recent changes in the dynamic properties of declining Arctic sea ice: A model study. Geophysical Research Letters, 39(20): L20503
    [60]
    Zhang Jinlun, Schweiger A, Steele M, et al. 2015. Sea ice floe size distribution in the marginal ice zone: Theory and numerical experiments. Journal of Geophysical Research: Oceans, 120(5): 3484–3498. doi: 10.1002/2015JC010770
    [61]
    Zuo Guangyu, Dou Yinke, Chang Xiaomin, et al. 2018a. Design and performance analysis of a multilayer sea ice temperature sensor used in polar region. Sensors, 18(12): 4467
    [62]
    Zuo Guangyu, Dou Yinke, Lei Ruibo. 2018b. Discrimination algorithm and procedure of snow depth and sea ice thickness determination using measurements of the vertical ice temperature profile by the ice-tethered buoys. Sensors, 18(12): 4162. doi: 10.3390/s18124162
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