2025
Boundary layer and mixing layer height: Models vs. Ground-based measurements intercomparison
JULAHA, Kajal; Vladimír ŽDÍMAL; Adéla HOLUBOVÁ ŠMEJKALOVÁ; Kateřina KOMÍNKOVÁ; Naděžda ZÍKOVÁ et. al.Základní údaje
Originální název
Boundary layer and mixing layer height: Models vs. Ground-based measurements intercomparison
Autoři
JULAHA, Kajal; Vladimír ŽDÍMAL; Adéla HOLUBOVÁ ŠMEJKALOVÁ; Kateřina KOMÍNKOVÁ (203 Česká republika, domácí) a Naděžda ZÍKOVÁ
Vydání
Atmospheric Research, Elsevier Ltd, 2025, 0169-8095
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10509 Meteorology and atmospheric sciences
Stát vydavatele
Spojené státy
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 4.400 v roce 2024
Organizační jednotka
Přírodovědecká fakulta
UT WoS
001400282600001
EID Scopus
2-s2.0-85213857935
Klíčová slova anglicky
Boundary layer; Mixing Layer; Ceilometer; Reanalysis; ERA5; HYSPLIT
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 5. 3. 2025 10:39, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
Detailed characterization of the planetary boundary layer (PBL) and mixing layer height (MLH) is essential for gaining insights into air quality, pollutant dispersion, and the dynamics of the lower atmosphere. This research involves MLH from four atmospheric models—ERA5 (European Centre for Medium-Range Weather Forecasts Reanalysis v5), Reanalysis, GDAS (Global Data Assimilation System), and GFS (Global Forecast System), representing diverse approaches commonly applied in atmospheric research, mainly in air quality studies. The intercomparison analyzes the simulated MLH from the models, comparing them with observations from radiosondes and ceilometers to capture diurnal and seasonal variations in boundary layer dynamics. The study reveals significant diurnal and seasonal variations, with a close alignment between ERA5 boundary layer and ceilometer mixing layer observations, Reanalysis consistently underestimating MLH altitude, and both GFS and GDAS models demonstrating reasonable diurnal cycles of MLH. During summer, all models underestimate MLH compared to ceilometer observations by 34–42 %, while in winter, overestimation relative to ceilometer observations ranges from 11 to 20 %. Factors contributing to this discrepancy, including meteorological variables and synoptic situations, were examined. GFS and GDAS tend to overestimate global radiation after 12:00 but underestimate MLH, while ERA5 consistently underestimated both radiation and MLH. Dependence in agreement between models and ceilometer observations was also observed for various synoptic situations. The interconnected nature of atmospheric stability and turbulence, highlighted by Richardson number analysis, further emphasizes the importance of understanding turbulence patterns for accurate MLH predictions.
Návaznosti
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