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A new regional mask for ice trends and climatologies

Walter N. Meier and J. Scott Stewart [email protected]

New 2021 Arctic mask History of old region masks Introduction Sea of Overall, Arctic is declining and Antarctic sea ice has a Bohai Japan Sea Original NASA Goddard mask near-zero trend over the past 40+ years. However, there are Pacific • Derived in mid-1980s by 1987 distinct regional variations in these trends. Regional masks were researchers at NASA Goddard developed to investigate these trends, but the masks were created • Modified in mid-1990s in a non-rigorous fashion for defined grids at low spatial resolution; Sea of • Derived on 25 km polar and there are inconsistencies in masks, even within products at Okhotsk stereographic grid NSIDC. Here we present an improved, more accurate regional • Based on accepted general 1995 mask based on accepted standards. definitions, but boundaries are not exact Bering • No coastal sea within Key features of new region mask Sea • Based off of International Hydrographic Office (IHO) • Combined Kara/ Laptev region definitions of – modified for use with sea ice, e.g.: Sea • Parkinson et al., JGR, 1999 • northern border at 76° N latitude, at southwest coast of St. Patrick Island Kara Sea Russia • Beaufort Sea northern border extends west at constant latitude Beaufort Central instead of diagonally across to as in IHO definition Sea Arctic Barents Modified NSIDC mask Sea Baltic • Regions defined initially as latitude/longitude vertices and of Sea • Uses Goddard mask as its Alaska mapped into GIS shapefiles foundation

Scandinavia • Subdivides some Goddard • Uses lines of constant latitude and longitude where reasonable East • Consistent, documented rules for connecting vertices and mapping Greenland regions into new regions Canadian Baffin • Separate Kara and Barents shapefile onto grids Archipelago Bay • Arctic Ocean split into 2007 • Flexible to facilitate gridded to different projections, spatial resolutions Beaufort, Chukchi, East Hudson • Region shapefile polygons drawn to overlap land to allow Bay Siberia, Laptev (coastal seas) Canada & use of different land masks • Northern boundary of coastal Labrador seas are arbitrary, drawn as • Consistency with previous region mask retained where it Sea straight lines in the projection makes sense Canada • Other regions and boundaries • New regions added for greater flexibility and broader same as Goddard mask applications • Meier et al., Ann. Glaciol., 2007 USA • , , , Gulf of St. Lawrence

MASIE mask Example: Beaufort Sea Beaufort Sea September Extent, 1979-2019 • Derived to support NSIDC Multi- 2007 Mask trend: -13,600 km2/year sensor Analyzed Sea Ice Extent Boundary displaced 2007 Mask (MASIE) product east of Pt. Barrow • Used NSIDC mask as basis, but Simple straight line boundary, Beaufort regions drawn independently varying latitude 2010 Sea • Regions created as shapefiles Boundary displaced manually drawn in GIS using Ad hoc northern boundary east of Bathurst straight lines on projection • , Bohai Sea, and Gulf IHO-defined boundary, 2021 Mask of Alaska regions added Pt. Barrow • Baffin and Gulf of St. Lawrence Constant latitude boundary, ~76° N, Beaufort Consistent with IHO 2021 Mask trend: -12,300 km2/year merged into one region Sea • Fetterer et al., 2010; NSIDC IHO-defined boundary, Cape Bathurst Sea ice data from NOAA/NSIDC Sea Ice Concentration Climate Data Record, Version 4 IHO-defined boundary, St. Patrick Island Meier et al., in press, https://nsidc.org/data/G02202/