Climatological Characteristics of Arctic and Antarctic Surface-Based Inversions*

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Climatology of the planetary boundary layer over the continental United States and Europe (2012, background): “boundary layers, which are common in midlatitude regions over land at night and in the winter, and at high latitudes [Zhang et al., 2011], is clearly a challenge for climate”
Mixed-phase clouds cause climate model biases in Arctic wintertime temperature inversions (2014, background): “Temperature inversions at high latitudes are a consequence of radiative cooling at the surface and advection of warmer air masses from lower latitudes (Zhang et al. 2011).”
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, unknown): “The temporal and spatial variations in BLH have been extensively assessed in previous studies at a regional or national scale, such as the contiguous United States (Seidel et al., 2012; Zhang et al., 2020a), Europe (Palarz et al ., 2018), Arctic and Antarctic (Zhang et al ., 2011), which are mainly ”