Estimating Vertical Wind Speeds: T_a, T_s, & P_a

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SUMMARY

Estimating vertical wind speeds using data from an automatic weather station (AWS) requires more than just surface temperature (T_s), air temperature (T_a), and air pressure (P_a). Key concepts such as eddy covariance and Bowen ratio energy balance are essential for understanding the relationship between evaporation and vertical air movement. The hypsometric equation can be utilized to calculate surface pressure, which may help relate pressure differences to vertical velocity. For in-depth knowledge, refer to the book "Evaporation Into the Atmosphere: Theory, History, and Applications" by W. Brutseart (1982).

PREREQUISITES
  • Eddy covariance methodology
  • Bowen ratio energy balance concepts
  • Hypsometric equation application
  • Understanding of atmospheric pressure dynamics
NEXT STEPS
  • Research the principles of eddy covariance for measuring vertical wind speeds
  • Study the Bowen ratio energy balance to understand its impact on evaporation and air movement
  • Learn how to apply the hypsometric equation in atmospheric studies
  • Read "Evaporation Into the Atmosphere: Theory, History, and Applications" by W. Brutseart for foundational knowledge
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Atmospheric scientists, meteorologists, and environmental researchers interested in estimating vertical wind speeds and understanding the dynamics of air movement related to temperature and pressure variations.

jones1234
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TL;DR
Calculate vertical wind speed based upon temperature difference
Hi all,

I have some data from an automatic weather station, with recordings of both 2m air temperature and 2m air pressure and also the surface temperature. Is it possible to estimate vertical wind speeds between the AWS and the surface based upon this data? Imagine T_a = 15 degrees and T_s = 30 degrees and P_a = 670 hPa. If not, which other variables do I need?

Thanks.
 
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It's more complicated than that. I suggest the these search terms to learn more: eddy covariance and Bowen ratio energy balance. These search terms are mostly about evaporation of surface water, and vertical air movement is closely tied to evaporation. A good book on the subject is Evaporation Into the Atmosphere: Theory, History, and Applications, by W. Brutseart (1982). An oldie, but goody, and it's still in print because it is the standard reference in that field: https://www.amazon.com/dp/9027712476/?tag=pfamazon01-20.
 
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jrmichler said:
It's more complicated than that. I suggest the these search terms to learn more: eddy covariance and Bowen ratio energy balance. These search terms are mostly about evaporation of surface water, and vertical air movement is closely tied to evaporation. A good book on the subject is Evaporation Into the Atmosphere: Theory, History, and Applications, by W. Brutseart (1982). An oldie, but goody, and it's still in print because it is the standard reference in that field: https://www.amazon.com/dp/9027712476/?tag=pfamazon01-20.
Thanks for the answer! I was thinking maybe to calculate the pressure at the surface with the hypsometric equation and then relate the pressure difference to a vertical velocity... is this also possible?
 

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