Gunilla Svensson
Gunilla Svensson
Professor, Stockholm University, Sweden
Verifierad e-postadress på misu.su.se - Startsida
Citeras av
Citeras av
Vertical structure of recent Arctic warming
RG Graversen, T Mauritsen, M Tjernström, E Källén, G Svensson
Nature 451 (7174), 53-56, 2008
Stable atmospheric boundary layers and diurnal cycles: challenges for weather and climate models
AAM Holtslag, G Svensson, P Baas, S Basu, B Beare, ACM Beljaars, ...
Bulletin of the American Meteorological Society 94 (11), 1691-1706, 2013
Single-column model intercomparison for a stably stratified atmospheric boundary layer
J Cuxart, AAM Holtslag, RJ Beare, E Bazile, A Beljaars, A Cheng, ...
Boundary-Layer Meteorology 118, 273-303, 2006
Quantifying climate feedbacks in polar regions
H Goosse, JE Kay, KC Armour, A Bodas-Salcedo, H Chepfer, D Docquier, ...
Nature communications 9 (1), 1919, 2018
Future climate change: modeling and scenarios for the Arctic
VM Kattsov, E Källén, HP Cattle, J Christensen, H Drange, ...
ACIA, 2005
Large‐scale circulation associated with moisture intrusions into the Arctic during winter
C Woods, R Caballero, G Svensson
Geophysical Research Letters 40 (17), 4717-4721, 2013
Advancing polar prediction capabilities on daily to seasonal time scales
T Jung, ND Gordon, P Bauer, DH Bromwich, M Chevallier, JJ Day, ...
Bulletin of the American Meteorological Society 97 (9), 1631-1647, 2016
Evaluation of the diurnal cycle in the atmospheric boundary layer over land as represented by a variety of single-column models: The second GABLS experiment
G Svensson, AAM Holtslag, V Kumar, T Mauritsen, GJ Steeneveld, ...
Boundary-Layer Meteorology 140, 177-206, 2011
Arctic climate change in 21st century CMIP5 simulations with EC-Earth
T Koenigk, L Brodeau, RG Graversen, J Karlsson, G Svensson, ...
Climate dynamics 40, 2719-2743, 2013
A total turbulent energy closure model for neutrally and stably stratified atmospheric boundary layers
T Mauritsen, G Svensson, SS Zilitinkevich, I Esau, L Enger, B Grisogono
Journal of the Atmospheric Sciences 64 (11), 4113-4126, 2007
Modelling the Arctic boundary layer: an evaluation of six ARCMIP regional-scale models using data from the SHEBA project
M Tjernström, M Žagar, G Svensson, JJ Cassano, S Pfeifer, A Rinke, ...
Boundary-layer meteorology 117, 337-381, 2005
Melt onset over Arctic sea ice controlled by atmospheric moisture transport
J Mortin, G Svensson, RG Graversen, ML Kapsch, JC Stroeve, ...
Geophysical Research Letters 43 (12), 6636-6642, 2016
Overview of the MOSAiC expedition: Atmosphere
MD Shupe, M Rex, B Blomquist, POG Persson, J Schmale, T Uttal, ...
Elem Sci Anth 10 (1), 00060, 2022
Review of wave‐turbulence interactions in the stable atmospheric boundary layer
J Sun, CJ Nappo, L Mahrt, D Belušić, B Grisogono, DR Stauffer, M Pulido, ...
Reviews of geophysics 53 (3), 956-993, 2015
Evaluation of limited-area models for the representation of the diurnal cycle and contrasting nights in CASES-99
GJ Steeneveld, T Mauritsen, EIF De Bruijn, JVG De Arellano, G Svensson, ...
Journal of Applied Meteorology and Climatology 47 (3), 869-887, 2008
Role of air-mass transformations in exchange between the Arctic and mid-latitudes
F Pithan, G Svensson, R Caballero, D Chechin, TW Cronin, AML Ekman, ...
Nature Geoscience 11 (11), 805-812, 2018
Observations of stably stratified shear-driven atmospheric turbulence at low and high Richardson numbers
T Mauritsen, G Svensson
Journal of the atmospheric sciences 64 (2), 645-655, 2007
Global distribution and seasonal variability of coastal low-level jets derived from ERA-Interim reanalysis
R Ranjha, G Svensson, M Tjernström, A Semedo
Tellus A: Dynamic Meteorology and Oceanography 65 (1), 20412, 2013
Consequences of poor representation of Arctic sea‐ice albedo and cloud‐radiation interactions in the CMIP5 model ensemble
J Karlsson, G Svensson
Geophysical Research Letters 40 (16), 4374-4379, 2013
The diurnal temperature range in the CMIP5 models
J Lindvall, G Svensson
Climate Dynamics 44, 405-421, 2015
Systemet kan inte utföra åtgärden just nu. Försök igen senare.
Artiklar 1–20