Search Results - "Persson, Ola G"
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1
The Critical Richardson Number and Limits of Applicability of Local Similarity Theory in the Stable Boundary Layer
Published in Boundary-layer meteorology (01-04-2013)“…Measurements of atmospheric turbulence made over the Arctic pack ice during the Surface Heat Budget of the Arctic Ocean experiment (SHEBA) are used to…”
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2
Continuous observations of the surface energy budget and meteorology over the Arctic sea ice during MOSAiC
Published in Scientific data (04-08-2023)“…The Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) was a yearlong expedition supported by the icebreaker R/V Polarstern ,…”
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3
Warm-air advection, air mass transformation and fog causes rapid ice melt
Published in Geophysical research letters (16-07-2015)“…Direct observations during intense warm‐air advection over the East Siberian Sea reveal a period of rapid sea‐ice melt. A semistationary, high‐pressure system…”
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4
Linking atmospheric synoptic transport, cloud phase, surface energy fluxes, and sea-ice growth: observations of midwinter SHEBA conditions
Published in Climate dynamics (01-08-2017)“…Observations from the Surface Heat Budget of the Arctic Ocean (SHEBA) project are used to describe a sequence of events linking midwinter long-range advection…”
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5
On the turbulent Prandtl number in the stable atmospheric boundary layer
Published in Boundary - layer meteorology (01-11-2007)“…This study focuses on the behaviour of the turbulent Prandtl number, Pr t , in the stable atmospheric boundary layer (SBL) based on measurements made during…”
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6
Surface energy budget responses to radiative forcing at Summit, Greenland
Published in The cryosphere (13-02-2017)“…Greenland Ice Sheet surface temperatures are controlled by an exchange of energy at the surface, which includes radiative, turbulent, and ground heat fluxes…”
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7
The Turbulent Structure of the Arctic Summer Boundary Layer During The Arctic Summer Cloud‐Ocean Study
Published in Journal of geophysical research. Atmospheres (27-09-2017)“…The mostly ice covered Arctic Ocean is dominated by low‐level liquid‐ or mixed‐phase clouds. Turbulence within stratocumulus is primarily driven by cloud top…”
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8
A transitioning Arctic surface energy budget: the impacts of solar zenith angle, surface albedo and cloud radiative forcing
Published in Climate dynamics (01-10-2011)“…Snow surface and sea-ice energy budgets were measured near 87.5°N during the Arctic Summer Cloud Ocean Study (ASCOS), from August to early September 2008…”
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9
Seasonal and latitudinal variations of surface fluxes at two Arctic terrestrial sites
Published in Climate dynamics (01-09-2018)“…This observational study compares seasonal variations of surface fluxes (turbulent, radiative, and soil heat) and other ancillary…”
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10
Application of TRMM PR and TMI Measurements to Assess Cloud Microphysical Schemes in the MM5 for a Winter Storm
Published in Journal of applied meteorology and climatology (01-06-2010)“…This paper uses observations from Tropical Rainfall Measuring Mission (TRMM) precipitation radar (PR) and microwave imager (TMI) to evaluate the cloud…”
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11
Parametrizing turbulent exchange over summer sea ice and the marginal ice zone
Published in Quarterly journal of the Royal Meteorological Society (01-04-2010)“…The surface of the Arctic Ocean in summer is a mix of sea ice and water in both leads and melt ponds. Here we use data collected at multiple sites during the…”
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12
SHEBA flux-profile relationships in the stable atmospheric boundary layer
Published in Boundary-layer meteorology (01-09-2007)“…Measurements of atmospheric turbulence made during the Surface Heat Budget of the Arctic Ocean Experiment (SHEBA) are used to examine the profile stability…”
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13
Low‐Level Baroclinic Jets Over the New Arctic Ocean
Published in Journal of geophysical research. Oceans (01-06-2018)“…During the Sea State cruise in the fall of 2015, in the Chukchi/Beaufort Sea region, there were five strong (>10 m s−1) surface wind events associated with…”
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14
Onset and end of the summer melt season over sea ice: thermal structure and surface energy perspective from SHEBA
Published in Climate dynamics (01-09-2012)“…Various measurements from the Surface Heat Flux of the Arctic Ocean (SHEBA) experiment have been combined to study structures and processes producing the onset…”
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15
The Potential of TerraSAR-X to Observe Wind Wave Interaction at the Ice Edge
Published in IEEE journal of selected topics in applied earth observations and remote sensing (01-06-2017)“…This paper performs a study on sea state and wind fields at the ice edge boundary by utilizing information from different sources including synthetic aperture…”
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Evaluation of atmospheric boundary layer-surface process relationships in a regional climate model along an East Antarctic traverse
Published in Journal of Geophysical Research: Atmospheres (15-05-2012)“…Some primary physical relationships related to the surface climate and atmospheric boundary layer were examined over East Antarctica and evaluated in the…”
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THE SUMMERTIME ARCTIC ATMOSPHERE: Meteorological Measurements during the Arctic Ocean Experiment 2001
Published in Bulletin of the American Meteorological Society (01-09-2004)“…An atmospheric boundary layer experiment into the high Arctic was carried out on the Swedish ice-breakerOdenduring the summer of 2001, with the primary…”
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18
Stable Boundary-Layer Scaling Regimes: The Sheba Data
Published in Boundary-layer meteorology (01-08-2005)“…Turbulent and mean meteorological data collected at five levels on a 20-m tower over the Arctic pack ice during the Surface Heat Budget of the Arctic Ocean…”
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19
Snowfall and snow accumulation during the MOSAiC winter and spring seasons
Published in The cryosphere (17-06-2022)“…Data from the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition allowed us to investigate the temporal dynamics of…”
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20
Outlier Problem in Evaluating Similarity Functions in the Stable Atmospheric Boundary Layer
Published in Boundary-layer meteorology (01-08-2012)“…The gradient-based similarity approach removes turbulent fluxes as governing parameters and replaces them with vertical gradients of mean wind speed and…”
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