From a low pressure-center the pressure increases by 1 kPa eastward across a distance of 1000 km. Assume standard atmosphere static stability (standard tropospheric lapse rate) above the top of the atmospheric boundary layer (ABL), calculate the vertical velocity out of the top of the boundary layer at 1000 krn. You may use the data from the table below. Parameter Value Density of air Coriolis parameter 1 kg m3 5x10 s Drag coefficient at the bottom Brunt-Vaisala frequency 0.002 0.015 s

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From a low pressure-center the pressure increases by 1 kPa eastward across a distance of 1000 km. Assume a
standard atmosphere static stability (standard tropospheric lapse rate) above the top of the atmospheric
boundary layer (ABL), calculate the vertical velocity out of the top of the boundary layer at 1000 krn.
You may use the data from the table below.
Parameter
Density of air
Coriolis parameter
Drag coefficient at the bottom
Brunt-Vaisala frequency
Value
1 kg m3
5x10's
0.002
0.015 s
Transcribed Image Text:From a low pressure-center the pressure increases by 1 kPa eastward across a distance of 1000 km. Assume a standard atmosphere static stability (standard tropospheric lapse rate) above the top of the atmospheric boundary layer (ABL), calculate the vertical velocity out of the top of the boundary layer at 1000 krn. You may use the data from the table below. Parameter Density of air Coriolis parameter Drag coefficient at the bottom Brunt-Vaisala frequency Value 1 kg m3 5x10's 0.002 0.015 s
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