Report written by Jim Doyle, Sunday, April 11
MISS was located at the Independence airport and documented a northerly low-level jet in the 1-2 km layer with a maximum near 25 m/s at 12 UTC and a deeper layer of northwesterly flow at 00 UTC 11 April.
The sounding launched from MAPR at 1200 UTC 10 April showed strong northerly flow present between 1 and 2 km (v component). A shallow stable layer was present near 650 mb and a nocturnal inversion was present at the surface.
MAPR documented northerly winds early on April 10. During the evening, the MAPR data was contaminated by migratory birds. A possible signature of wave activity was apparent in the MAPR vertical velocity data in the time period 17-21 UTC 10 April. Periods of rising and sinking motion that were coherent in time were present in the low-levels at MAPR during this time period.
The surface network indicated weak flow near 12 UTC and as the solar radiation increased after sunrise, the strong northerlies were mixed downward. Gusty northerly winds were present in Owens Valley with most surface stations indicating sustained winds greater than 20 mph for a period of time in the morning with peak gusts around 36 mph. A second period of strong northerly winds at the surface occurred at around 00 UTC 11 April.