Sentences with phrase «gridded sea ice concentrations»

Parkinson, C. L., Comiso, J. C. & Zwally, H. J. Nimbus - 5 ESMR polar gridded sea ice concentrations.

Not exact matches

Yuan et al. (LDEO Columbia University), 5.08 (+ / - 0.51), Statistical The prediction is made by statistical models, which are capable to predict Arctic sea ice concentrations at grid points 3 - month in advance with reasonable skills.

Arctic sea ice extent reconstruction - Kinnard et al. 2011 Sea ice albedo feedback - NASA Polar jet stream - NC State University Greenland ice sheet surface melt - NASA Permafrost distribution in the Arctic - GRID - Arendal Atmospheric methane concentration - NOAA ESRL Russia plants flag at North Pole - Reutsea ice extent reconstruction - Kinnard et al. 2011 Sea ice albedo feedback - NASA Polar jet stream - NC State University Greenland ice sheet surface melt - NASA Permafrost distribution in the Arctic - GRID - Arendal Atmospheric methane concentration - NOAA ESRL Russia plants flag at North Pole - ReutSea ice albedo feedback - NASA Polar jet stream - NC State University Greenland ice sheet surface melt - NASA Permafrost distribution in the Arctic - GRID - Arendal Atmospheric methane concentration - NOAA ESRL Russia plants flag at North Pole - Reuters

Remember: You do not need any more than 15 % concentration of sea ice in a «grid cell» to be counted in the extent value.

A look at Arctic sea ice concentration over the last 100 years (through 2013) using the latest NSIDC gridded 1850 - reconstruction from Walsh et al. [2016].

HadISST is a unique combination of monthly globally - complete fields of SST and sea ice concentration on a 1 degree latitude - longitude grid from 1870 to date.

The following maps show the probability of encountering September sea ice at concentrations greater than 15 % (corresponding to ice extent as commonly defined) in a particular grid cell.

September Sea Ice Probability (SIP, the probability of sea ice concentration > 15 % at each grid cell), in the Slater, NRL - SSC / Metzger et al., and MetOffice / Peterson et al. forecasSea Ice Probability (SIP, the probability of sea ice concentration > 15 % at each grid cell), in the Slater, NRL - SSC / Metzger et al., and MetOffice / Peterson et al. forecasIce Probability (SIP, the probability of sea ice concentration > 15 % at each grid cell), in the Slater, NRL - SSC / Metzger et al., and MetOffice / Peterson et al. forecassea ice concentration > 15 % at each grid cell), in the Slater, NRL - SSC / Metzger et al., and MetOffice / Peterson et al. forecasice concentration > 15 % at each grid cell), in the Slater, NRL - SSC / Metzger et al., and MetOffice / Peterson et al. forecasts.

The primary sources of the post-1972 data are the hemispheric fields of sea - ice concentration from (1) the U.S. National Ice Center (NIC), whose weekly grids (derived primarily from satellite data) span the period 1972 - 1994, and (2) the satellite passive - microwave grids from the Scanning Multichannel Microwave Radiometer (SMMR) / Special Sensor Microwave / Imager (SSM / I) period, 1978 - 97 (Parkinson and others, 199ice concentration from (1) the U.S. National Ice Center (NIC), whose weekly grids (derived primarily from satellite data) span the period 1972 - 1994, and (2) the satellite passive - microwave grids from the Scanning Multichannel Microwave Radiometer (SMMR) / Special Sensor Microwave / Imager (SSM / I) period, 1978 - 97 (Parkinson and others, 199Ice Center (NIC), whose weekly grids (derived primarily from satellite data) span the period 1972 - 1994, and (2) the satellite passive - microwave grids from the Scanning Multichannel Microwave Radiometer (SMMR) / Special Sensor Microwave / Imager (SSM / I) period, 1978 - 97 (Parkinson and others, 1999).

Gridded Monthly Sea Ice Extent and Concentration, 1850 Onward, Version 1.