On the Potential of 25 Years (1991–2015) of Rawinsonde Measurements for Elucidating Climatological and Spatiotemporal Patterns of Afternoon Boundary Layer Depths over the Contiguous US

<div>Percent of times, 1 Jan 1991 through 31 Dec 2015, when there is a near-surface (&lt;100 m) inversion present in the IGRA 0000 UTC sounding (a). Panel (b) shows the local time of 0000 UTC sounding illustrating the four different time zones in the study region.</div>

Advances in Meteorology

fig3

Figure 3

Figure 3: On the Potential of 25 Years (1991–2015) of Rawinsonde Measurements for Elucidating Climatological and Spatiotemporal Patterns of Afternoon Boundary Layer Depths over the Contiguous US 

Figure 3 | On the Potential of 25 Years (1991–2015) of Rawinsonde Measurements for Elucidating Climatological and Spatiotemporal Patterns of Afternoon Boundary Layer Depths over the Contiguous US 