Biblio
Filters: First Letter Of Last Name is I [Clear All Filters]
Eddy-current interactions using a quasi-geostrophic model. Mesoscale/ synoptic coherent structures in geophysical turbulence 277 -291 (1989).
Reference Quality Upper-Air Measurements: guidance for developing GRUAN data products. Atmospheric Measurement Techniques 3, 1217-1231 (2010).
On the effect of a sill on dense water formation in a marginal sea. Journal of Marine Research 66, 325-345 (2008). Abstract
Download: ISS_JMR2008.pdf (758.05 KB)
On the Nordic Sea's Role in the Atlantic Meridional Overturning Circulation. Doctoral Thesis No. 67 (2007).
Passive Microwave sea ice retrievals and validation. 11th Biennial Conference of Pan Ocean Remote Sensing (PORSEC) - 2012 (2012).
Comparison of the Arctic sea ice extent and area time series obtained from different algorithms for sea ice concentration using passive microwave sensor data. Arctic Science Summit Week (2009). Download: Ivanova_Johannessen09.pdf (42.1 KB)
Error assessment of satellite-derived lead fraction in the Arctic. The Cryosphere 10, (2016). Download: ivanova_etal_2016_error_assessment_of_satellite-derived_lead_fraction_in_the_arctic.pdf (2.64 MB)
Sea ice concentration and thickness variability from passive microwave and altimetry measurements during the last 2-3 decades. Climate Change in High Latitudes Bjerknes Centre 10-years Anniversary Conference (2012).
Arctic sea ice variability observed by satellite passive microwave sensors: sea ice algorithms comparison. IPY - OsloScience Conference (2010). Download: Poster.pdf (14.73 MB)
Arctic sea ice variability observed by satellite passive microwave sensors: sea ice algorithms comparison. World Climate Research Programme workshop on seasonal to multi-decadal predictability of polar climate (2010). Download: Poster.pdf (14.73 MB)
Retrieval of arctic sea ice parameters by satellite passive microwave sensors: A comparison of eleven sea ice concentration algorithms. IEEE Transactions on Geoscience and Remote Sensing 52, (2014).
Radar imaging of sea surface at marginal ice zone and leads in Barents and Kara seas. Norwegian-Russian collaboration in Svalbard (2006).
