Biblio
Filtre: First Letter Of Title er C [Slett Alle Filtre]
Calculation of the height of stable boundary layers in practical applications. Boundary-layer Meteorology 389-409 (2002).på <http://www.springerlink.com/content/100245/?p=43e84a3972f3443fbe3e13aeb2578da0&pi=0>
Calibration of sea ice dynamic parameters in an ocean-sea ice model using an ensemble Kalman filter. Journal of Geophysical Research (JGR): Oceans 119, (2014).
Cap rock fracture analysis, Well 7228/2 1. Structural Geology Croup, GI, UiB/NERSC Report no. 6, 16pp (1990).
Cap rock frature analysis, Well 7321/9 1. Revised version with fracture log. Structural Geology Croup GI, UiB/NERSC, Report no. 3 34 (1990).
Capabilities of Remote Sensing as a source of operative objective information about the polar sea ice cover state. Oceanograpy and Sea Ice 19 (2011).
The carbon cycle in the Greenland Sea ESOP-2 Final Report. GEOS, Univ. i Bergen to EC FP4 (1999).
Carbon Dioxide Sequestration in the Ocean: The Possibility Of Injection in Shallow Water. Energy Conversion Management 33, 697-704 (1992).
Carbon uptake by the ocean, subject to biological feedback. Arctic Science Summit Week (2009). Abstract
A Case Study for the ocean co2 injection experiment on Hawaii. NERSC Technical Report no. 185 (2000).
Case Study of a Coastal jet at Spitsbergen - Comparison of SAR- and model-estimated wind. Monthly Weather Review 130, 1040-1051 (2002).
Causes of the large warm bias in the Angola–Benguela Frontal Zone in the Norwegian Earth System Model. Climate Dynamics (2017).doi:10.1007/s00382-017-3896-2
A Cautionary Note on the Use of the Kolmogorov-Smirnov Test for Normality. Monthly Weather Review 135, 1151-1157 (2007).
Certain aspects of high-latitude climate variability. 188 (2014).
Ch. 2: Our Changing Climate. Climate Change Impacts in the United States: The third National Climate Assessment (2014).doi:10.7930/J0KW5CXT
Ch. 6 Interaction with the global climate system. Arctic Climate Change The ACSYS Decade and Beyond (2012).
Challenges and capabilities of data assimilation. Nansen-Tutu Centre Scientific Opening Symposium (2011).
The change in sea ice cover is responsible for non-uniform variation in winter temperature over East Asia. Atmospheric and Oceanic Science Letters 8, (2015).
Changes in past, present and future sea level, focusing on the Norwegian west coast. NGF symposium (2010).
Changes in past, present and future sea level, focusing on the Norwegian west coast. MARE Climate Forum (2010).
Changes in the Arctic sea ice cover from passive microwave satellite measurements. Proceedings of Scientific Conference High Latitude Seas and Marine Cryosphere , 25 27 October 2007, St. Petersburg, Russia (2007).
Changes in the Arctic Sea Ice Cover in the Twentieth and Twenty-First Centuries. Sea Ice in the Arctic, Past, Present and Future (2020).doi:10.1007/978-3-030-21301-5_4
