Abstract

Sea-ice concentration (SIC) data with fine spatial resolution and spatially continuous coverage are needed, for example, for estimating heat fluxes. Passive microwave measurements of the Advanced Scanning Microwave Radiometer 2 (AMSR2) offer spatial continuity, but are limited to spatial resolutions of 5 km and coarser. Thermal infrared data of the Moderate Resolution Imaging Spectroradiometer (MODIS) provide a spatial resolution of 1 km, but are limited to cloud-free scenes. We exploit the benefits of both and present a merged SIC dataset with 1 km spatial resolution and spatially continuous coverage for the Arctic. MODIS and AMSR2 SIC are retrieved separately and then merged by tuning the MODIS SIC to preserve the mean AMSR2 SIC. We first evaluate the variability of the dynamically retrieved MODIS ice tie-point. Varying the starting position of the area used for the tie-point retrieval changes the MODIS SIC by on average 1.9%, which we mitigate by considering different starting positions and using the average as ice tie-point. Furthermore, the SIC datasets are evaluated against a reference dataset derived from Sentinel-2A/B reflectances between February and May 2019. We find that the merged SIC are 1.9% smaller than the reference SIC if thin ice is considered as ice and 4.9% higher if thin ice is considered as water. There is only a slight bias (0.3%) between the MODIS and the merged SIC; however, the root mean square deviation of 5% indicates that the two datasets do yield different results. In an example of poor-quality MODIS SIC, we identify an unscreened cloud and high ice-surface temperature as reasons for the poor quality. Still, the merged SIC are of similar quality as the passive microwave SIC in this example. The benefit of merging MODIS and AMSR2 data is demonstrated by showing that the finer resolution of the merged SIC compared to the AMSR2 SIC allows an enhanced potential for the retrieval of leads. At the same time, the data are available regardless of clouds. Last, we provide uncertainty estimates. The MODIS and merged SIC uncertainty are between 5% and 10% from February to April and increase up to 25% (merged SIC) and 35% (MODIS SIC) in May. They are identified as conservative uncertainty estimates.

Highlights

  • The Arctic region is of high importance for the Earth’s climate

  • How sensitive is the merged sea-ice concentration towards the choice of the Moderate Resolution Imaging Spectroradiometer (MODIS) ice tie-point? Choosing an arbitrary starting position for the ice temperature background field used as ice tie-point introduces a Sea-ice concentration (SIC) uncertainty of 1.9%, which is mitigated by varying the starting position and taking the average of 48 iterations as ice tie-point

  • The standard deviation within these 48 iterations serves as uncertainty estimate for the MODIS ice tie-point

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Summary

Introduction

The Arctic region is of high importance for the Earth’s climate. Its influence extends far outside the polar regions and affects the weather in the mid-latitudes as well as the global radiative budget. Sea-ice concentration (SIC), the fraction of a given ocean area covered by sea ice, has been monitored from space since 1972 with the Electrically Scanning Microwave Radiometer (ESMR) and routinely since 1979 with two-daily Arctic-wide coverage until 1987 and daily Arctic-wide coverage from 1987 onwards. The spatial resolutions of the first passive microwave radiometers were about 50 km of the 19 GHz and 25 km of the 37 GHz channels of the Scanning Multichannel Microwave Radiometer (SMMR). Spatial resolutions of the 89 GHz channels of the Advanced Microwave Scanning Radiometer 2 (AMSR2), which are used in this study, are less than 5 km. The resolutions are given here as the instantaneous field of view

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