Comparison of summer Arctic sea ice surface temperatures from <i>in situ</i> and MODIS measurements

Na Li; Bingrui Li; Ruibo Lei; Qun Li

doi:10.1007/s13131-020-1644-7

Volume 39 Issue 9

Sep. 2020

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Article Navigation > Acta Oceanologica Sinica > 2020 > 39(9): 18-24

Na Li, Bingrui Li, Ruibo Lei, Qun Li. Comparison of summer Arctic sea ice surface temperatures from in situ and MODIS measurements[J]. Acta Oceanologica Sinica, 2020, 39(9): 18-24. doi: 10.1007/s13131-020-1644-7

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Na Li, Bingrui Li, Ruibo Lei, Qun Li. Comparison of summer Arctic sea ice surface temperatures from in situ and MODIS measurements[J]. Acta Oceanologica Sinica, 2020, 39(9): 18-24. doi: 10.1007/s13131-020-1644-7

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Comparison of summer Arctic sea ice surface temperatures from in situ and MODIS measurements

doi: 10.1007/s13131-020-1644-7

Na Li^{1, 2
,
,},
Bingrui Li^{1, 2},
Ruibo Lei^{1, 2},
Qun Li^{1, 2}

1.
Polar Research Institute of China, Shanghai 200136, China
2.
MNR Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai 200136, China

Funds: The National Natural Science Foundation of China under contract No. 41606222; the National Key Research and Development Project under contract No. 2016YFC1400303.

More Information

Corresponding author: E-mail: lina@pric.org.cn
Received Date: 2019-10-26
Accepted Date: 2019-11-18

Available Online: 2020-12-28

Publish Date: 2020-09-25

Abstract

Abstract

Ship-borne infrared radiometric measurements conducted during the Chinese National Arctic Research Expedition (CHINARE) in 2008, 2010, 2012, 2014, 2016 and 2017 were used for in situ validation studies of the Moderate Resolution Imaging Spectroradiometer (MODIS) sea ice surface temperature (IST) product. Observations of sea ice were made using a KT19.85 radiometer mounted on the Chinese icebreaker Xuelong between July and September over six years. The MODIS-derived ISTs from the satellites, Terra and Aqua, both show close correspondence with ISTs derived from radiometer spot measurements averaged over areas of 4 km×4 km, spanning the temperature range of 262–280 K with a ±1.7 K (Aqua) and ±1.6 K (Terra) variation. The consistency of the results over each year indicates that MODIS provides a suitable platform for remotely deriving surface temperature data when the sky is clear. Investigation into factors that cause the MODIS IST bias (defined as the difference between MODIS and KT19.85 ISTs) shows that large positive bias is caused by increased coverage of leads and melt ponds, while large negative bias mostly arises from undetected clouds. Thin vapor fog forming over Arctic sea ice may explain the cold bias when cloud cover is below 20%.
- sea ice surface temperature,
- thermal radiometer,
- MODIS,
- Arctic Ocean

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References

[1]	Comiso J C. 2010. Polar Oceans from Space. New York: Springer-Verlag, 495, doi: 10.1007/978-0-387-68300-3
[2]	Comiso J C. 2012. Large decadal decline of the Arctic multiyear ice cover. Journal of Climate, 25(4): 1176–1193. doi: 10.1175/JCLI-D-11-00113.1
[3]	Dozier J, Warren S G. 1982. Effect of viewing angle on the infrared brightness temperature of snow. Water Resource Research, 18(5): 1424–1434. doi: 10.1029/WR018i005p01424
[4]	Eicken H, Grenfell T C, Perovich D K, et al. 2004. Hydraulic controls of summer Arctic pack ice albedo. Journal of Geophysical Research: Oceans, 109(C8): C08007. doi: 10.1029/2003JC001989
[5]	Haggerty J A, Maslanik J A, Curry J A. 2003. Heterogeneity of sea ice surface temperature at SHEBA from aircraft measurements. Journal of Geophysical Research: Oceans, 108(C10): 8052. doi: 10.1029/2000JC000560
[6]	Hall D K, Box J E, Casey K A, et al. 2008. Comparison of satellite-derived and in-situ observations of ice and snow surface temperatures over Greenland. Remote Sensing of Environment, 112(10): 3739–3749. doi: 10.1016/j.rse.2008.05.007
[7]	Hall D K, Comiso J C, Digirolamo N E, et al. 2012. A satellite-derived climate-quality data record of the clear-sky surface temperature of the Greenland ice sheet. Journal of Climate, 25(14): 4785–4798. doi: 10.1175/JCLI-D-11-00365.1
[8]	Hall D K, Key J R, Casey K A, et al. 2004. Sea ice surface temperature product from MODIS. IEEE Transactions on Geoscience and Remote Sensing, 42(5): 1076–1087. doi: 10.1109/TGRS.2004.825587
[9]	Hall D K, Nghiem S V, Rigor I G, et al. 2015. Uncertainties of temperature measurements on snow-covered land and sea ice from in situ and MODIS data during Bromex. Journal of Applied Meteorology and Climatology, 54(5): 966–978. doi: 10.1175/JAMC-D-14-0175.1
[10]	Kearns E J, Hanafin J A, Evans R H, et al. 2000. An independent assessment of Pathfinder AVHRR sea surface temperature accuracy using the Marine Atmosphere Emitted Radiance Interferometer (MAERI). Bulletin of the American Meteorological Society, 81(7): 1525–1536. doi: 10.1175/1520-0477(2000)081<1525:AIAOPA>2.3.CO;2
[11]	Key J R, Collins J B, Fowler C, et al. 1997. High-latitude surface temperature estimates from thermal satellite data. Remote Sensing of Environment, 61(2): 302–309. doi: 10.1016/S0034-4257(97)89497-7
[12]	Key J R, Maslanik J A, Papakyriakou T, et al. 1994. On the validation of satellite-derived sea ice surface temperature. Arctic, 47(3): 280–287. doi: 10.14430/arctic1298
[13]	Koenig L S, Hall D K. 2010. Comparison of satellite, thermochron and air temperatures at Summit, Greenland, during the winter of 2008/09. Journal of Glaciology, 56(198): 735–741. doi: 10.3189/002214310793146269
[14]	Laxon S W, Giles K A, Ridout A L, et al. 2013. CryoSat-2 estimates of Arctic sea ice thickness and volume. Geophysical Research Letters, 40(4): 732–737. doi: 10.1002/grl.50193
[15]	Lei Ruibo, Li Zhijun, Li Na, et al. 2012. Crucial physical characteristics of sea ice in the Arctic section of 143°–180°W during August and early September 2008. Acta Oceanologica Sinica, 31(4): 65–75. doi: 10.1007/s13131-012-0221-0
[16]	Lindsay R W, Rothrock D A. 1994. Arctic sea ice surface temperature from AVHRR. Journal of Climate, 7(1): 174–183. doi: 10.1175/1520-0442(1994)007<0174:ASISTF>2.0.CO;2
[17]	Markus T, Stroeve J C, Miller J. 2009. Recent changes in Arctic sea ice melt onset, freezeup, and melt season length. Journal of Geophysical Research: Oceans, 114(C12): C12024. doi: 10.1029/2009JC005436
[18]	Minnett P J. 2003. Radiometric measurements of air-sea and air-ice temperature differences in the Arctic. In: 2003 IEEE International Geoscience and Remote Sensing Symposium. Toulouse, France: IEEE, doi: 10.1109/IGARSS.2003.1293748
[19]	Pan Zengdi. 2015. The report of 2014 Chinese Arctic Research Expedition (in Chinese). Beijing: China Ocean Press, 96–100
[20]	Perovich D K, Jones K F, Light B, et al. 2011. Solar partitioning in a changing Arctic sea-ice cover. Annals of Glaciology, 52(57): 192–196. doi: 10.3189/172756411795931543
[21]	Radionov V F, Bryazgin N N, Alexandrov E I. 1997. The Snow Cover of the Arctic Basin. Seattle, WA: Applied Physics Laboratory, University of Washington
[22]	Riggs G A, Hall D K. 2015. MODIS sea ice products user guide to Collection 6, https://landweb.modaps.eosdis.nasa.gov/QA_WWW/forPage/user_guide/MODISC6SeaIceproductsUserguide.pdf [2015-3-17/2019-5-1].
[23]	Scambos T A, Haran T M, Massom R. 2006. Validation of AVHRR and MODIS ice surface temperature products using in situ radiometers. Annals of Glaciology, 44: 345–351. doi: 10.3189/172756406781811457
[24]	Schweiger A J. 2004. Changes in seasonal cloud cover over the Arctic seas from satellite and surface observations. Geophysical Research Letters, 31(12): L12207. doi: 10.1029/2004GL020067
[25]	Shuman C A, Hall D K, Digirolamo N E, et al. 2014. Comparison of near-surface air temperatures and MODIS ice-surface temperatures at summit, Greenland (2008-13). Journal of Applied Meteorology and Climatology, 53(9): 2171–2180. doi: 10.1175/JAMC-D-14-0023.1
[26]	Wenny B N, Xiong X, Madhavan S. 2012. Evaluation of Terra and Aqua MODIS thermal emissive band calibration consistency. In: Proceedings Volume 8533, Sensors, Systems, and Next-Generation Satellites XVI. Edinburgh, United Kingdom: SPIE, doi: 10.1117/12.974230
[27]	Worby A P, Geiger C, Paget M J, et al. 2008. Thickness distribution of Antarctic sea ice. Journal of Geophysical Research: Oceans, 113(C5): C05S92. doi: 10.1029/2007JC004254
[28]	Xia Wentao, Xie Hongjie, Ke Changqing. 2014. Assessing trend and variation of Arctic sea-ice extent during 1979-2012 from a latitude perspective of ice edge. Polar Research, 33(1): 21249. doi: 10.3402/polar.v33.21249
[29]	Xie Simei, Xue Zhenhe, Jiang Dezhong, et al. 2001. Summer Arctic sea fog. Acta Oceanologica Sinica, 20(2): 183–196
[30]	Yu Y, Rothrock D A, Lindsay R W. 1995. Accuracy of sea ice temperature derived from the advanced very high resolution radiometer. Journal of Geophysical Research: Oceans, 100(C3): 4525–4532. doi: 10.1029/94JC02244