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...

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Extracted 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 krm. 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