Investigation of near-global daytime boundary layer height using high-resolution radiosondes: first results and comparison with ERA5, MERRA-2, JRA-55, and NCEP-2 reanalyses
<p>The planetary boundary layer (PBL) governs the vertical transport of mass, momentum, and moisture between the surface and the free atmosphere, and thus the determination of PBL height (BLH) is recognized as crucial for air quality, weather, and climate analysis. Although reanalysis products...
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| Autores principales: | , , , , , , , , , , , , , , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Copernicus Publications
2021
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/8d0c75d44d424e0da8a232398d63aa2e |
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| Sumario: | <p>The planetary boundary layer (PBL) governs the vertical transport of mass,
momentum, and moisture between the surface and the free atmosphere, and thus
the determination of PBL height (BLH) is recognized as crucial for air
quality, weather, and climate analysis. Although reanalysis products can
provide important insight into the global view of BLH in a seamless way, the BLH observed in situ on a global scale remains poorly understood due to the lack of
high-resolution (1 or 2 s) radiosonde measurements. The present study
attempts to establish a near-global BLH climatology at synoptic times (00:00
and 12:00 UTC) and in the daytime using high-resolution radiosonde
measurements over 300 radiosonde sites worldwide for the period 2012 to
2019, which is then compared against the BLHs obtained from four reanalysis
datasets, including ERA5, MERRA-2, JRA-55, and NCEP-2. The variations in
daytime BLH exhibit large spatial and temporal dependence, and as a result
the BLH maxima are generally discerned over the regions such as the western
United States and western China, in which the balloon launch times mostly
correspond to the afternoon. The diurnal variations in BLH are revealed with
a peak at 17:00 local solar time (LST). The most promising reanalysis product
is ERA5, which underestimates BLH by around 130 m as compared to radiosondes
released during daytime. In addition, MERRA-2 is a well-established product
and has an underestimation of around 160 m. JRA-55 and NCEP-2 might produce
considerable additional uncertainties, with a much larger underestimation of
up to 400 m. The largest bias in the reanalysis data appears over the
western United States and western China, and it might be attributed to the
maximal BLH in the afternoon when the PBL has risen. Statistical analyses
further indicate that the biases of reanalysis BLH products are positively
associated with orographic complexity, as well as the occurrence of static
instability. To our best knowledge, this study presents the first
near-global view of high-resolution radiosonde-derived boundary layer<span id="page17080"/> height
and provides a quantitative assessment of the four frequently used
reanalysis products.</p> |
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