Climatology of the planetary boundary layer over the continental United States and Europe

Although boundary layer processes are important in climate, weather and air quality, boundary layer climatology has received little attention, partly for lack of observational data sets. We analyze boundary layer climatology over Europe and the continental U.S. using a measure of boundary layer heig...

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Veröffentlicht in:Journal of Geophysical Research: Atmospheres 2012-09, Vol.117 (D17), p.n/a
Hauptverfasser: Seidel, Dian J., Zhang, Yehui, Beljaars, Anton, Golaz, Jean-Christophe, Jacobson, Andrew R., Medeiros, Brian
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container_issue D17
container_start_page
container_title Journal of Geophysical Research: Atmospheres
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creator Seidel, Dian J.
Zhang, Yehui
Beljaars, Anton
Golaz, Jean-Christophe
Jacobson, Andrew R.
Medeiros, Brian
description Although boundary layer processes are important in climate, weather and air quality, boundary layer climatology has received little attention, partly for lack of observational data sets. We analyze boundary layer climatology over Europe and the continental U.S. using a measure of boundary layer height based on the bulk Richardson number. Seasonal and diurnal variations during 1981–2005 are estimated from radiosonde observations, a reanalysis that assimilates observations, and two contemporary climate models that do not. Data limitations in vertical profiles introduce height uncertainties that can exceed 50% for shallow boundary layers (
doi_str_mv 10.1029/2012JD018143
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We analyze boundary layer climatology over Europe and the continental U.S. using a measure of boundary layer height based on the bulk Richardson number. Seasonal and diurnal variations during 1981–2005 are estimated from radiosonde observations, a reanalysis that assimilates observations, and two contemporary climate models that do not. Data limitations in vertical profiles introduce height uncertainties that can exceed 50% for shallow boundary layers (&lt;1 km) but are generally &lt;20% for deeper boundary layers. Climatological heights are typically &lt;1 km during daytime and &lt;0.5 km at night over both regions. Seasonal patterns for daytime and nighttime differ; daytime heights are larger in summer than winter, but nighttime heights are larger in winter. The four data sets show similar patterns of spatial and seasonal variability but with biases that vary spatially, seasonally, and diurnally. Compared with radiosonde observations, the reanalysis and the climate models produce deeper layers due to difficulty simulating stable conditions. The higher‐time‐resolution reanalysis reveals the diurnal cycle in height, with maxima in the afternoon, and with amplitudes that vary seasonally (larger in summer) and regionally (larger over western U.S. and southern Europe). The lower‐time‐resolution radiosonde data and climate model simulations capture diurnal variations better over Europe than over the U.S., due to differences in local sampling times. Key Points New 25 year PBL climatology shows diurnal, seasonal, and spatial structures Two climate models and one reanalysis show PBL climates similar to radiosondes Shallow nighttime and winter PBL heights are more uncertain, too high in models</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1029/2012JD018143</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Air quality ; Atmospheric sciences ; Boundary layers ; Climate change ; Climate models ; Climatology ; Diurnal variations ; Earth ; Earth sciences ; Earth, ocean, space ; Europe ; Exact sciences and technology ; Geophysics ; mixing height ; planetary boundary layer ; Seasonal variations ; Summer ; Troposphere ; United States ; Winter</subject><ispartof>Journal of Geophysical Research: Atmospheres, 2012-09, Vol.117 (D17), p.n/a</ispartof><rights>2012. 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Geophys. Res</addtitle><description>Although boundary layer processes are important in climate, weather and air quality, boundary layer climatology has received little attention, partly for lack of observational data sets. We analyze boundary layer climatology over Europe and the continental U.S. using a measure of boundary layer height based on the bulk Richardson number. Seasonal and diurnal variations during 1981–2005 are estimated from radiosonde observations, a reanalysis that assimilates observations, and two contemporary climate models that do not. Data limitations in vertical profiles introduce height uncertainties that can exceed 50% for shallow boundary layers (&lt;1 km) but are generally &lt;20% for deeper boundary layers. Climatological heights are typically &lt;1 km during daytime and &lt;0.5 km at night over both regions. Seasonal patterns for daytime and nighttime differ; daytime heights are larger in summer than winter, but nighttime heights are larger in winter. The four data sets show similar patterns of spatial and seasonal variability but with biases that vary spatially, seasonally, and diurnally. Compared with radiosonde observations, the reanalysis and the climate models produce deeper layers due to difficulty simulating stable conditions. The higher‐time‐resolution reanalysis reveals the diurnal cycle in height, with maxima in the afternoon, and with amplitudes that vary seasonally (larger in summer) and regionally (larger over western U.S. and southern Europe). The lower‐time‐resolution radiosonde data and climate model simulations capture diurnal variations better over Europe than over the U.S., due to differences in local sampling times. 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Geophys. Res</addtitle><date>2012-09-16</date><risdate>2012</risdate><volume>117</volume><issue>D17</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-897X</issn><eissn>2156-2202</eissn><eissn>2169-8996</eissn><abstract>Although boundary layer processes are important in climate, weather and air quality, boundary layer climatology has received little attention, partly for lack of observational data sets. We analyze boundary layer climatology over Europe and the continental U.S. using a measure of boundary layer height based on the bulk Richardson number. Seasonal and diurnal variations during 1981–2005 are estimated from radiosonde observations, a reanalysis that assimilates observations, and two contemporary climate models that do not. Data limitations in vertical profiles introduce height uncertainties that can exceed 50% for shallow boundary layers (&lt;1 km) but are generally &lt;20% for deeper boundary layers. 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Key Points New 25 year PBL climatology shows diurnal, seasonal, and spatial structures Two climate models and one reanalysis show PBL climates similar to radiosondes Shallow nighttime and winter PBL heights are more uncertain, too high in models</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2012JD018143</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record>
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identifier ISSN: 0148-0227
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subjects Air quality
Atmospheric sciences
Boundary layers
Climate change
Climate models
Climatology
Diurnal variations
Earth
Earth sciences
Earth, ocean, space
Europe
Exact sciences and technology
Geophysics
mixing height
planetary boundary layer
Seasonal variations
Summer
Troposphere
United States
Winter
title Climatology of the planetary boundary layer over the continental United States and Europe
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