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Mesoscale Variability in the Summer Arctic Boundary Layer
by
Mauritsen, Thorsten
, Tjernström, Michael
in
air
/ Air masses
/ Arctic
/ Arctic boundary layer
/ Arctic climate
/ Arctic region
/ Atmosfärs- och hydrosfärsvetenskap
/ Atmosphere and hydrosphere sciences
/ Atmospheric boundary layer
/ Atmospheric Sciences
/ Boundaries
/ Boundary layer
/ Boundary layers
/ Boundary-layer clouds
/ Clouds
/ Convection, turbulence, diffusion. Boundary layer structure and dynamics
/ cooling
/ Ducted buoyancy waves
/ Earth and Environmental Science
/ Earth Sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ External geophysics
/ Fluid dynamics
/ Fluid flow
/ Geovetenskap
/ gravity
/ Gravity waves
/ ice
/ Mesoscale
/ Mesoscale circulation
/ Mesoscale fronts
/ Meteorologi
/ Meteorology
/ NATURAL SCIENCES
/ NATURVETENSKAP
/ Original Paper
/ Pack ice
/ Summer
/ temperature
/ troposphere
/ Turbulence
/ Turbulent flow
/ variance
/ wavelet
2009
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Mesoscale Variability in the Summer Arctic Boundary Layer
by
Mauritsen, Thorsten
, Tjernström, Michael
in
air
/ Air masses
/ Arctic
/ Arctic boundary layer
/ Arctic climate
/ Arctic region
/ Atmosfärs- och hydrosfärsvetenskap
/ Atmosphere and hydrosphere sciences
/ Atmospheric boundary layer
/ Atmospheric Sciences
/ Boundaries
/ Boundary layer
/ Boundary layers
/ Boundary-layer clouds
/ Clouds
/ Convection, turbulence, diffusion. Boundary layer structure and dynamics
/ cooling
/ Ducted buoyancy waves
/ Earth and Environmental Science
/ Earth Sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ External geophysics
/ Fluid dynamics
/ Fluid flow
/ Geovetenskap
/ gravity
/ Gravity waves
/ ice
/ Mesoscale
/ Mesoscale circulation
/ Mesoscale fronts
/ Meteorologi
/ Meteorology
/ NATURAL SCIENCES
/ NATURVETENSKAP
/ Original Paper
/ Pack ice
/ Summer
/ temperature
/ troposphere
/ Turbulence
/ Turbulent flow
/ variance
/ wavelet
2009
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Do you wish to request the book?
Mesoscale Variability in the Summer Arctic Boundary Layer
by
Mauritsen, Thorsten
, Tjernström, Michael
in
air
/ Air masses
/ Arctic
/ Arctic boundary layer
/ Arctic climate
/ Arctic region
/ Atmosfärs- och hydrosfärsvetenskap
/ Atmosphere and hydrosphere sciences
/ Atmospheric boundary layer
/ Atmospheric Sciences
/ Boundaries
/ Boundary layer
/ Boundary layers
/ Boundary-layer clouds
/ Clouds
/ Convection, turbulence, diffusion. Boundary layer structure and dynamics
/ cooling
/ Ducted buoyancy waves
/ Earth and Environmental Science
/ Earth Sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ External geophysics
/ Fluid dynamics
/ Fluid flow
/ Geovetenskap
/ gravity
/ Gravity waves
/ ice
/ Mesoscale
/ Mesoscale circulation
/ Mesoscale fronts
/ Meteorologi
/ Meteorology
/ NATURAL SCIENCES
/ NATURVETENSKAP
/ Original Paper
/ Pack ice
/ Summer
/ temperature
/ troposphere
/ Turbulence
/ Turbulent flow
/ variance
/ wavelet
2009
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Journal Article
Mesoscale Variability in the Summer Arctic Boundary Layer
2009
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Overview
Observations from the summer Arctic Ocean Experiment 2001 (AOE-2001) are analysed with a focus on the interactions between mesoscale and boundary-layer dynamics. Wavelet analyses of surface-pressure variations show daylong periods with different characteristics, some featuring episodes of pronounced high-frequency surface-pressure variability, here hypothesized to be caused by trapped gravity waves. These episodes are accompanied by enhanced boundary-layer turbulence and an enhanced spectral gap, but with only minor influence on the surface stress. During these episodes, mesoscale phenomena were often encountered and usually identified as front-like features in the boundary layer, with a peak in drizzle followed by changing temperature. These phenomena resemble synoptic fronts, though they are generally shallow, shorter-lasting, have no signs of frontal clouds, and do not imply a change in air mass. Based on this analysis, we hypothesize that the root cause of the episodes with high-frequency surface-pressure variance are shallow, mesoscale fronts moving across the pack ice. They may be formed due to local-to-regional horizontal contrasts, for example, between air with different lifetimes over the Arctic or with perturbations in the cloud field causing differential cooling of the boundary layer. Thermal contrasts sharpen as the air is transported with the mean flow. The propagating mesoscale fronts excite gravity waves, which affect the boundary-layer turbulence and also seem to favour entrainment of free tropospheric air into the boundary layer.
Publisher
Dordrecht : Springer Netherlands,Springer Netherlands,Springer,Springer Nature B.V
Subject
/ Arctic
/ Atmosfärs- och hydrosfärsvetenskap
/ Atmosphere and hydrosphere sciences
/ Clouds
/ Convection, turbulence, diffusion. Boundary layer structure and dynamics
/ cooling
/ Earth and Environmental Science
/ Exact sciences and technology
/ gravity
/ ice
/ Pack ice
/ Summer
/ variance
/ wavelet
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