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Old December 20th 17, 03:20 AM posted to rec.aviation.soaring
Michael Opitz
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Posts: 318
Default How does sun heat the air?

At 02:28 20 December 2017, wrote:
The people who really care about this stuff are climatologists (and
climate=
modelers), and increasingly the solar power community. The

issue as far
a=
s the soaring community is concerned is that most of the sunlight

that is
l=
ost to absorption in the atmosphere is mostly-always lost=20

* UV is absorbed in the stratosphere; as far as total energy is

concerned
=
there is not much variability in what gets to the ground. =20

* Chappuis-band O3 absorption (in the visible red) can change the

surface
=
heat flux a few percent, no more

* the big H2O band at 940 nm is very important climatologically ..

but is
p=
erhaps 5% of total energy flux and not as variable as people might

think=20

* H2O and CO2 (and some others) at wavelengths 1.4 microns

lead to
substa=
ntial extinctions in the 1.4 - 3 micron wavelength domains -- but

our
huma=
n eyes don't see that, the sun's solar output is decreasing at longer
wavel=
engths, nor do silicon solar cells get energy from these

wavelengths. =20

When you look at energy balance commonly more than 20% of the

sun's
radiati=
on is absorbed in the atmosphere, and this is very important to the
thermal=
structure of the atmosphere, but it isn't highly variable (as a

fraction
o=
f total energy) so people just don't pay too much attention to it,

for
purp=
oses like soaring.

This energy ends up as heat, distributed non-uniformly through the
atmosphe=
ric column. The most blatantly obvious effect is that we have a
stratosphe=
re; there are also climatically-important consequences to this in

the
trop=
osphere. Most of this heat is deposited at altitudes where we

don't fly.
=
=20

The dominant issues that effect lower-boundary layer heating rates

are
pret=
ty obvious: clouds! Yes, surface-albedo ... and then a very large

factor
n=
ot discussed here is what meteorologists call the "Bowen ratio:"

the ratio
=
of the latent-to-sensible heat flux from the surface ... how much of

the
he=
at is used to evaporate water.

Deserts are good for soaring because most of the captured

radiation does
go=
to sensible heat. =20

A "secret" most western pilots don't know -- the best soaring

season in
th=
e northeast is spring, before the trees leaf out. It's our desert.

After
=
they leaf out ... then every damned tree is a water-sucking

nuisance ...
an=
d a subtle point is that deciduous trees flux more water than

conifers ...
=
there are easily-observable differences in Bowen-ratio from

deciduous vs
co=
nifer forests. =20

More subtly there is a second "good" period in the fall when the

trees
lose=
their leaves, although with the declining sunlight it's not really

great.
=
But since the time of Benjamin Franklin naturalists noted that

stream
flow=
s in the northeast jump after the trees lose their leaves in the fall,

and
=
correctly attributed the reason for this.

One of several reasons "the high ground" is usually better soaring
(everywh=
ere) is that water runs off it; the trees are almost always water-

stress
li=
mited and shifted to species (conifers) that do that better. A
water-stres=
sed tree keeps its stomata closed: doesn't flux water but also

cannot
photo=
synthesize.=20

Plants do change the surface albedo, usually lower it. Plants look

green
b=
ecause they don't use green light, and they want to reflect it to

avoid
its=
heat. They also increase the albedo at longer wavelengths. But

this
eff=
ect on albedo is usually less important that their water flux ... if

they
a=
ren't water stressed.

Soil moisture can be measured (sort-of) by remote sensing in the
microwave,=
and there are very large variations in soil moisture temporally

(ask any
f=
armer), but also spatially across the terrain ... in places (not our
wester=
n deserts) where there's enough water for plants to grow

generously. =20

Hey Eric Greenwell? You still flying around Richland Washington? I

flew
w=
ith you, and towed you years ago when I worked at PNL. It's

pretty arid
ou=
t there ... but nobody finds good thermals coming up off the big

irrigated
=
crop circles. In desert terrains stay away from green like the

plague.

In the northeast the hierarchy is plowed-fields better than conifers,
conif=
ers better than growing hay or corn UNLESS the farmers are

complaining
abou=
t a dry spell, say out of the river bottoms and anywhere with

deciduous
tre=
es, worse yet willows. =20


Thanks for a great post!

RO