Use the Simplified Penman Monteith equation (eq. f) to calculate actual evaporation (E₂) in Philadelphia on May 30th. Note that you will need to calculate A as part of the equation. I have also provided the equation for A on the attached document. **Note on units. Since the simplified version of the equation has already multiplied various constants (all with different units), you do not need to include the units in those values (the 0.408 and 105.028 values). However, please include the other units in your initial writing of the equation.
Use the Simplified Penman Monteith equation (eq. f) to calculate actual evaporation (E₂) in Philadelphia on May 30th. Note that you will need to calculate A as part of the equation. I have also provided the equation for A on the attached document. **Note on units. Since the simplified version of the equation has already multiplied various constants (all with different units), you do not need to include the units in those values (the 0.408 and 105.028 values). However, please include the other units in your initial writing of the equation.
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Location: just outside of Philadelphia, Pennsylvania -latitude 40° N
Date: May 30, 2019-Julian date= day 150
Temperature (T): 21° C
000
Relative humidity (RH): 0.8
Maximum number of bright sunshine hours per day (N) = 14 hours
Actual recorded number of bright sunshine hours per day (n) = 10 hours
Land cover: grassland
Aerodynamic resistance (ra) = 60 s/m for grassland
Surface resistance (rs) = 50 s/m for grassland
Albedo = 0.23 for grassland
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