about
Vertical structure of recent Arctic warming.MEAD: an interdisciplinary study of the marine effects of atmospheric deposition in the Kattegat.Warm-air advection, air mass transformation and fog causes rapid ice meltThe Arctic Summer Cloud Ocean Study (ASCOS): overview and experimental designThe thermodynamic structure of summer Arctic stratocumulus and the dynamic coupling to the surfaceCloud and boundary layer interactions over the Arctic sea ice in late summerMeteorological conditions in the central Arctic summer during the Arctic Summer Cloud Ocean Study (ASCOS)A transitioning Arctic surface energy budget: the impacts of solar zenith angle, surface albedo and cloud radiative forcingMeasurements of bubble size spectra within leads in the Arctic summer pack iceThe Turbulence Structure of the Stable Atmospheric Boundary Layer Around a Coastal Headland: Aircraft Observations and Modelling ResultsStable Atmospheric Boundary Layers and Diurnal Cycles: Challenges for Weather and Climate ModelsArctic climate change in 21st century CMIP5 simulations with EC-EarthInfluence of the Arctic Oscillation on the vertical distribution of clouds as observed by the A-Train constellation of satellitesThe vertical distribution of thin features over the Arctic analysed from CALIPSO observationsModelling micro- and macrophysical contributors to the dissipation of an Arctic mixed-phase cloud during the Arctic Summer Cloud Ocean Study (ASCOS)Measurement of wind profiles by motion-stabilised ship-borne Doppler lidarThe importance of spring atmospheric conditions for predictions of the Arctic summer sea ice extentOn the potential contribution of open lead particle emissions to the central Arctic aerosol concentrationModelling atmospheric structure, cloud and their response to CCN in the central Arctic: ASCOS case studiesModelling coastal low-level wind-jets: does horizontal resolution matter?Structure and variability of the Oman coastal low-level jetGlobal distribution and seasonal variability of coastal low-level jets derived from ERA-Interim reanalysisAn evaluation of Arctic cloud and radiation processes during the SHEBA year: simulation results from eight Arctic regional climate modelsEvaluation of an ensemble of Arctic regional climate models: spatiotemporal fields during the SHEBA yearEvaluation of an ensemble of Arctic regional climate models: spatiotemporal fields during the SHEBA yearAerosol composition and sources in the central Arctic Ocean during ASCOSThe Turbulent Structure of the Arctic Summer Boundary Layer During The Arctic Summer Cloud-Ocean StudyWarm winds from the Pacific caused extensive Arctic sea-ice melt in summer 2007Mesoscale Variability in the Summer Arctic Boundary LayerGraversen et al. replyClimate impact of deforestation over South Sudan in a regional climate modelOn the fog variability over south AsiaAtmospheric mass-transport inconsistencies in the ERA-40 reanalysisAdvances in understanding and parameterization of small-scale physical processes in the marine Arctic climate system: a reviewResponse of the lower troposphere to moisture intrusions into the ArcticThe vertical structure of cloud radiative heating over the Indian subcontinent during summer monsoonThe free troposphere as a potential source of arctic boundary layer aerosol particlesDirect determination of the air-sea CO2 gas transfer velocity in Arctic sea ice regionsClouds, warm air, and a climate cooling signal over the summer ArcticLagrangian tracing of Sahelian Sudan moisture sources
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Zweeds onderzoeker
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Michael Tjernström
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