Solving Earth Science Problem: Surface Energy Balance

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SUMMARY

The discussion focuses on solving the surface energy balance equation, represented as Q¤ = QH + QE + QG, where QH is sensible heat, QE is latent heat, and QG is ground heat flux. Participants emphasize the importance of interpreting the components of the equation and computing 24-hour totals for each heat transfer type based on provided data from Alberta's grassland. The conversation suggests that understanding the notation and performing calculations for part b is essential before tackling part a, which simplifies the interpretation process.

PREREQUISITES
  • Understanding of surface energy balance concepts
  • Familiarity with heat transfer terminology (sensible heat, latent heat, ground heat flux)
  • Basic knowledge of data interpretation from tables
  • Proficiency in performing calculations with units (J/m², kg/m², mm/m²)
NEXT STEPS
  • Learn how to compute daily totals for energy balance components using real data
  • Study the implications of each component (QH, QE, QG) in environmental science
  • Explore methods for measuring and analyzing surface energy balance in different ecosystems
  • Investigate the role of soil moisture in energy balance calculations
USEFUL FOR

Environmental scientists, researchers in earth sciences, and students studying surface energy balance and heat transfer in ecosystems will benefit from this discussion.

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I've no idea how to start this question, please take a look.
I just pick some of the data from the table.
Thanks very much.

Daily cycle in the surface energy balance
The surface energy balance states that
Q¤ = QH + QE + QG
where QH is sensible heat, QE is latent heat and QG is ground heat flux.
I'm required to
a) give a brief interpretation1
b) compute these 24 hour totals2
– transfer of sensible heat to the atmosphere in [Jm¡2]
– transfer of latent heat to the atmosphere in [Jm¡2]
– transfer of water to the atmosphere expressed in [kgm¡2]
– equivalent loss of stored soil liquid water expressed in [mmm¡2] (note: the conversion factor is the density of liquid water, i.e. 1000 kgm¡3)

Table: Daily cycle in hourly-averaged energy balance components over grassland in Alberta. 1 July 2003. (All fluxes in W m¡2)
hour Q¤ QG QH QE
1 -77 -17 -117 23
2 -68 -17 -67 11
. . . . .
. . . . .
24 -66 -15 -101 19
etc.
 
Last edited:
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Step one is to communicate the meanings of "G, H, E" which are presumably subscripts of Q --- saves people "guessing" notations. Step two is take a stab at "part b;" once you've got "b" in hand, "a" is trivial. Dunno why they asked things in the backward order, but that's what's left you with "no idea."
 

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