A aviation & planes forum. AviationBanter

If this is your first visit, be sure to check out the FAQ by clicking the link above. You may have to register before you can post: click the register link above to proceed. To start viewing messages, select the forum that you want to visit from the selection below.

Go Back   Home » AviationBanter forum » rec.aviation newsgroups » Soaring
Site Map Home Register Authors List Search Today's Posts Mark Forums Read Web Partners

How does sun heat the air?



 
 
Thread Tools Display Modes
Prev Previous Post   Next Post Next
  #32  
Old December 20th 17, 03:20 AM posted to rec.aviation.soaring
Michael Opitz
external usenet poster
 
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


 




Thread Tools
Display Modes

Posting Rules
You may not post new threads
You may not post replies
You may not post attachments
You may not edit your posts

vB code is On
Smilies are On
[IMG] code is On
HTML code is Off
Forum Jump

Similar Threads
Thread Thread Starter Forum Replies Last Post
Lotsa Heat Maple1 Aviation Photos 2 August 7th 07 03:21 AM
Carb Heat vlado Piloting 9 January 22nd 07 03:08 PM
But it's a dry heat.... Casey Wilson Piloting 31 July 23rd 05 10:09 PM
Pre-Heat at BED? Colin W Kingsbury Owning 7 January 21st 05 02:25 AM
auxiliary heat Jim Burns Owning 15 October 20th 04 09:08 PM


All times are GMT +1. The time now is 05:32 AM.


Powered by vBulletin® Version 3.6.4
Copyright ©2000 - 2025, Jelsoft Enterprises Ltd.
Copyright 2004-2025 AviationBanter.
The comments are property of their posters.