Zum Inhalt Springen
Home
General
Guides
Reviews
News
Welcome
Maps & Data
Go to overview: Maps & data
Satellite data
Go to overview: Satellite data
Sea-ice concentration
Go to overview: Sea-ice concentration
Maps of sea-ice concentration
Sea-ice extent time series/
trend curves
Sea-ice edge comparison
Multiyear ice
Animations of sea-ice concentration
Sea-ice thickness
Go to overview: Sea-ice thickness
CryoSat-2 (AWI)
CryoSat-2/SMOS (AWI)
SMOS (AWI)
SMOS (IUP)
Animations of sea-ice thickness
Sea-ice drift
Go to overview: Sea-ice drift
OSI-405-b
OSI-405-AMSR
OSI-405-multi
CERSAT-merged
CERSAT-AMSR
KIMURA
NSIDC
Sea-ice age
Buoys/Moorings
Go to overview: Buoys/
Moorings
Buoys
Moorings
Expedition data
Go to overview: Expedition data
Airborne measurements
Manual measurements
Echosounder data
MOSAiC data
Go to overview: MOSAiC
Sea-ice concentration with Polarstern's track
Sea-ice edge comparison with Polarstern's track
Multi-sattelite product for MOSAiC
Drift scenarios during MOSAiC
Ship radar
Drift forcasts during MOSAiC expedition
Ice Charts from National Ice Services
MOSAiC buoys
Sea-ice concentration (IUP Bremen)
CONTRASTS data
Go to overview: CONTRASTS 2025
Interactive viewer
Live data from the RV Polarstern
Expedition news
Regime 1: future Arctic
Regime 2: today's Arctic
Regime 3: past Arctic
Comparison of regime 1-3
Buoys from CONTRASTS 2025
Climatological data
Go to overview: Climatological data
Sea surface temperature anomaly
Temperature anomaly at 925 mbar
Sea level pressure anomaly
Precipitable water-content anomalies
Modelling data
Go to overview: Modelling data
CMIP5 sea-ice concentration
CMIP6 sea-ice concentration
Historical sea-ice data
Go to overview: Historical sea-ice data
Atlas of Antarctic sea-ice drift
Citation
Interactive maps
Go to overview: Interactive Maps
Annual cycle
Create your own animation
Sea-ice GIS
Maps & Data
Satellite data
Sea-ice thickness
CryoSat-2 (AWI)
Akruti 70 Oriya Keyboard Layout Pdf Portable Guide
These are applied after a consonant. On your PDF, highlight this table in yellow.
Back to top