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CASIWAL Presentation NO.10
Abstract: The Arctic sea ice cover is reducing rapidly, which has strong local climate impacts but also remote effects over the Eurasian continent. Results will be presented... -
CASIWAL Presentation NO.9
Abstract: Landfast ice is nearly immobile sea ice attached to the coast.Landfast ice inhibits atmo- sphere-ocean fluxes of heat moisture, and momentumleads to offshore flaw... -
CASIWAL Presentation NO.8
Abstract: The polar ice sheets are a large store of freshwater in the global climate system.The Ant arctic and Greenland lce Sheets have an approximate water equivalent of 57m... -
CASIWAL Presentation NO.7
Abstract: Variations in Arctic sea ice are not only apparent in the extent and thickness but also in its inter nal properties.The microstructure of summer Arctic sea ice changes... -
CASIWAL Presentation NO.6
The thesis can be found: https://helda.helsinki.fi/handle/10138/339471 The thesis consists following articles: I) Naakka T., et al.,, 2018, Arctic humidity inversions:... -
CASIWAL Presentation NO.5
Abstract: Antarctic sea ice shows a great importance in the heat exchange between ocean and atmosphere in the Southern hemisphere, and the variations of sea ice would reflect... -
CASIWAL Presentation NO.4
Abstract: Arctic sea ice is a vital indicator of global environment change, influencing the Earth’s surface energy balance, air-sea heat and mass exchange, atmospheric... -
CASIWAL Presentation NO.3
Abstract: Strong offshore wind events (SOWEs) occur frequently near the Antarctic coast during austral winter. These wind events are typically associated with passage of... -
CASIWAL Presentation NO.2
Abstract： Interactions between the land surface and climate are complex as a range of physical, chemical and biological processes take place. Changes in the land surface or... -
CASIWAL Presentation NO.1
Abstract： In this study, sea ice concentration (SIC) budgets were calculated for five ocean-sea ice reanalyses (CFSR, C-GLORSv7, GLORYS12v1, NEMO-EnKF and ORAS5), in the... -
Arctic sea ice drifting buoy（2018.01-2018.09）
Starting points: 76.998, 179.130 End point: 81.771, 168.588 Roughly covered sea: the East Siberian Sea Buoy number: 300234062559750 -
Arctic sea ice drifting buoy（2018.02-2018.08）
Starting points: 72.119, -139.730 End points: 73.332, -169.653 Roughly covered sea: Beaufort Sea Buoy number: 300234065164080 -
Arctic sea ice drifting buoy（2019.1-2019.12）
Buoy number: 300234066036110 Starting point: 74.425, -137.130 End: 75.481, -170.394 Approximate sea coverage: Beaufort Sea -
Arctic sea ice drifting buoy（2019.01-2019.08）
Buoy number: 300234065494020 Starting point: 74.774, -148.631 End point: 73.015, -137.530 Approximate sea coverage: Beaufort Sea -
Arctic sea ice drifting buoy（2019.01-2019.12）
Buoy number: 300234062880820 Starting point: 78.320, -167.886 End point: 83.562, -151.835 Approximate sea coverage: the central region of the Arctic -
Arctic sea ice drifting buoy（2020.01-2020.04）
Buoy number: 174640 Starting points: 79.743, 65.388 End: 76.380, 56.401 Approximate sea coverage: Barents Sea -
Arctic sea ice drifting buoy（2020.09-2020.11）
Buoy number: 300534060210350 Starting point: 78.880, -158.499 End point: 81.387, -158.309 Approximate sea coverage: Beaufort Sea -
MODIS daily cloud-free snow cover products over Tibetan Plateau
Snow cover over Tibetan Plateau plays an important role in regional water andenergy circulation. Snow ablation also affects downstream rivers. Snow parameters and their longterm...
