Biblio
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Interrisk ontologies (revised). (2008).
Benchmarking CMIP5 models with a subset of ESA CCI Phase 2 data using the ESMValTool. Remote Sensing of Environment 203, (2017).
Annual and seasonal fCO(2) and air-sea CO2 fluxes in the Barents Sea. Journal of Marine Systems 113-114, (2013).
Version 2 of the EUMETSAT OSI SAF and ESA CCI sea-ice concentration climate data records. The Cryosphere 13, (2019).
The international surface temperature initiative's global land surface databank. AIP Conference Proceedings (2013).doi:10.1063/1.4821420 Abstract
Sea Ice Observations. Chapter 8 in Mass balance of the cryosphere: Observations and modeling of contemporary and future changes. 337-392 (2004).
Ontologies and ontology extension for marine environmental information systems. ENVIP 2010 Workshop 679, 8 (2010). Abstract
A Framework for the Development, Design and Implementation of a Sustained Arctic Ocean Observing System. Frontiers in Marine Science (2019).
Net primary productivity estimates and environmental variables in the Arctic Ocean: An assessment of coupled physical-biogeochemical models. Journal of Geophysical Research (JGR): Oceans 121, (2016).
Data assimilation and Inverse Methods in Terms of a Probabilistic Formulation. Monthly Weather Review 124, 2898-2913 (1996).
The impact of ensemble filter definition on the assimilation of temperature profiles in the tropical Pacific. Quarterly Journal of the Royal Meteorological Society 131, 3291-3300 (2005). Abstract
An improved and homogeneous altimeter sea level record from the ESA Climate Change Initiative. Earth System Science Data 10, (2018).
Sea Ice Physics and Modelling. (2017).
Arctic Climate Change The ACSYS Decade and Beyond. 464 (2012).
ESA ice sheet CCI: derivation of the optimal method for surface elevation change detection of the Greenland ice sheet – round robin results. International Journal of Remote Sensing 36, (2015).
Modulation of Aleutian Low and Antarctic Oscillation co-variability by ENSO. Climate Dynamics 44, (2015).
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).
Modulation of Aleutian Low and Antarctic Oscillation co-variability by ENSO. Climate Dynamics (2014).doi:10.1007/s00382-014-2134-4
Atlantic multidecadal oscillation modulates the impacts of Arctic sea ice decline. Geophysical Research Letters 45, (2018).