Biblio
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Northeast Atlantic sea surface circulation during the past 30-10 14C kyr. Paleoceanography 616-625 (1999).
Interrisk ontologies (revised). (2008).
Multi-model ensemble mean of global climate models fails to reproduce early twentieth century Arctic warming. Polar Science 30, (2021).
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
Download: enfip2010_paper11.pdf (332.74 KB)
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).
A Framework for the Development, Design and Implementation of a Sustained Arctic Ocean Observing System. Frontiers in Marine Science (2019).
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
Sea Ice Physics and Modelling. Sea Ice Analysis and Forecasting - Towards an Increased Reliance on Automated Prediction Systems (2017).
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).
Arctic sea-ice loss intensifies aerosol transport to the Tibetan Plateau. Nature Climate Change 10, (2020).
Modulation of Aleutian Low and Antarctic Oscillation co-variability by ENSO. Climate Dynamics (2014).doi:10.1007/s00382-014-2134-4
Stratospheric precursor of non-uniform variation in early spring surface temperature over Eurasia. Journal of Meteorological Research 31, (2017).
