Diurnal variations of the planetary boundary layer observed with an L-band clear-air doppler radar

Details Diurnal variations of the planetary boundary layer observed with an L-band clear-air doppler radar Diurnal variations of the planetary boundary layer observed with an L-band clear-air doppler radar

Jun 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995bolme..74..419h&link_type=abstract

Boundary-Layer Meteorology, Volume 74, Issue 4, pp.419-424

Physics

3

Scientific paper

Based on continuous observations of the planetary boundary layer (PBL) with an L-band (1357.5 MHz) boundary-layer radar (BLR) at a hilly location in Japan, we have discovered that on clear days, a thin enhanced echo layer corresponding to the top of the PBL (or mixed layer) appeared at about 500 m height in the morning and ascended to about 1500 m in the afternoon. Strong upward velocities were observed below the echo layer (or inside the PBL), reaching 1500 m in the afternoon.

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