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June 1996 MABL speed, temperatureEach profiler below has a time series for June of:Top: Virtual temperature (C) vs Z from profiler Middle: Speed (m/s) vs Z from profiler Bottom: Air-sea temperature difference from NDBC buoy nearest the profiler To my eye, the air-sea temperature difference from the NDBC buoys is often correlated with the MABL height: as the MABL is increasingly stable, it is often increasingly shallow. The temperature difference and the MABL height seem to change on the same ~10 day scale. Newport
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| Note that the boundary layer appears to warm as it moves from the northern to the southern stations, where the diurnal signal is more apparent. A 5-10 day cycle seems to be apparent in the southern stations. Over the course of June the MABL appears to deepen, then thin abruptly. | ![]() |
Newport
06
06
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08
09
10
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16
17
25
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Cresent City
06
06
07
08
09
10
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22
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Point Arena
06
06
07
08
09
10
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18
18
22
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Bodega Bay
06
06
07
08
09
10
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Fort Ord (to 4km)
06
06
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Fort Ord (to 1500m) 06
06
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Ft Ord time series 06
06
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08
08
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13
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Piedras Blancas
06
06
07
08
09
10
12
13
14
15
16
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22
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Goleta Bay
06
06
07
08
09
10
12
13
14
15
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18
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The data on this page is unpublished. If it is used please cite the author Kathleen Edwards, the Center for Coastal Studies, and the Coastal Waves group at Scripps Insitution of Oceanography.