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

By D. Seidel, Yehui Zhang, Anton Beljaars, J. Golaz, A. Jacobson, B. Medeiros. 2012

425 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/74197297956bf0e5ec55baa22d5b1bfcebe644f4

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Igor Esau
2. Axel Von Engeln
3. Sergej Zilitinkevich
4. Ad Stoffelen
5. João Paulo Ramos Teixeira
6. Sungsu Park

In Global and Planetary Change

1. Axel Von Engeln
2. João Paulo Ramos Teixeira
3. Sergej Zilitinkevich
4. Sungsu Park

Citations in the corpus

• Diurnal asymmetry to the observed global warming (2017, background): “37: 79–93 (2017) on behalf of the Royal Meteorological Society. therefore under-estimating temperature trends (Seidel et al., 2012; Davy and Esau, 2014).”
• Determination and climatology of the planetary boundary layer height above the Swiss plateau by in situ and remote sensing measurements as well as by the COSMO-2 model (2014, methodology): “The seasonal cycle of the nocturnal SBL was only addressed on the basis of temperature (T ) profiles from RS measurements (Seidel et al., 2010, 2012; Beyrich and Leps, 2012).”
• Investigation of near-global daytime boundary layer height using high-resolution radiosondes: First results and comparison with ERA-5, MERRA-2, JRA-55, and NCEP-2 reanalyses (2021, positive): “It is well known to be influenced by radiative cooling at night and by downward solar radiation reaching the ground surface at daytime, respectively, forming a stable boundary layer (SBL) and convective boundary layer (CBL), with a typical PBL depth (BLH) of less than 500 m and 1–3 km (Zhang et al.,”
• A Planetary Boundary Layer Height Climatology Derived from ECMWF Reanalysis Data (2013, background): “Teixeira et al. (2011) analyzed over 20 weather and climate prediction models and showed, for example, that cloud-top and PBL height model results at 208N in the stratocumulus-to-cumulus transition region along the GPCI transect can basically be anywhere between 1 and 3 km. Nevertheless, there have ”