that climate thing
DESCRIPTION
That Climate Thing. 1. Atmospheric Circulation. Atmosphere. is the Earth’s 110 km thick gaseous envelope, and evolved in three stages:. 4-4.5 Ga ago dominantly H, He (much like Jupiter, Saturn and Sun) 3.5 Ga ago changed to mostly C, N and O when the first oceans appeared - PowerPoint PPT PresentationTRANSCRIPT
![Page 1: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/1.jpg)
1. Atmospheric Circulation
![Page 2: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/2.jpg)
Thermosphere
MesosphereStratosphereTroposphere
300 km
50 km
40 km10 km
400 km altitude
Exosphere
is the Earth’s 110 km thick gaseous envelope, andevolved in three stages:
4-4.5 Ga agodominantly H, He (much like Jupiter, Saturn and Sun)
3.5 Ga ago changed to mostly C, N and O when the first oceans appeared
1.25 Ga agobecame mostly N and O, as at the present time, because of loss of C. Where did this atmospheric
CO2 go? It ended up in the oceans. How? Because of
photosynthesis.
![Page 3: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/3.jpg)
Troposphere
extends to 16-18 km above the tropics but <10 km above the poles;
contains ~80% of atmosphere’s mass; and
runs the hydrological cycle because tropo-spheric temperatures decrease with height.
Stra
tosp
he
reS
trato
sph
ere
StratopauseStratopause
Me
so
sph
ere
Me
so
sph
ere
MesopauseMesopause
Th
ermo
-T
herm
o-
sp
he
res
ph
ere
TropopauseTropopause
TroposphereTroposphere
Average temperature, °C
Hei
gh
t, a
bo
ve m
ean
sea
lev
el (
km)
Average atmospheric temperature
What if the tropo-spheric temperature
gradient changes?
Why is ozone good overAntarctica but bad over Southern California?
There is a hole in the Ozone layer right above Antarctica
![Page 4: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/4.jpg)
Sun is so far that we can assume Sun’s rays striking the Earth’s surface to be parallel. Because of the curvature of
Earth’s surface, then, solar heat input varies with latitude.
Sam
e in
pu
t
Tropics thus receive most solar heat per unit area
and the polar region the least.
![Page 5: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/5.jpg)
Why seasons?
Earth's spin axis tilts 23.5° from the vertical. Thus, as Earth completes is orbit, North pole tilts towards the Sun one-half the time, with peak at the Summer Solstice, whereas South pole tilts towards the Sun during the other half, with peak at Winter Solstice. Tropics, bounded by Tropic of Cancer (23.5°N) and Tropic of Capricorn (23.5°S), receive Sun all year round and therefore have no seasons, whereas temperate latitudes have seasons. Also, the northern temperate region (23.5°N to 66.5°N or the Arctic Circle) has summer when the southern temperate region (23.5°S to 66.5°S or the Antarctic Circle) has winter, and vice versa. What if Earth's spin axis became nearly vertical, as is the case with Venus? Will we still have the seasons?
What if Earth's spin axis became vertical, much like what exists on Venus? Will we still have the seasons?
![Page 6: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/6.jpg)
Differential heating:Tropics receive most solar heat.Differential gravity:Gravitational acceleration is most at the poles, least at the equator. Differential rotation:Equatorial surface wind blows to the west, against the direction of Earth’s spin.
A general model of tropospheric circulation3 forces govern this circulation:
![Page 7: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/7.jpg)
The Patterns in Global Air Circulation
![Page 8: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/8.jpg)
30° N
60° N
30° S
60° N
0°
Rotation has consequences for Weather
Because of rotation, surface air blows increasingly to the west the closer we approach the equator.
This is Coriolis effect and is demonstrated in the followinganimation.
![Page 9: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/9.jpg)
Majo
r surface w
ind
pattern
s
![Page 10: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/10.jpg)
http://web1.umkc.edu/sites/env-sci/module4/weblab4.htm
Satellite images of particles (aerosols) in the atmosphere are one way to illustrate the path of global atmospheric circulation. The animation below shows daily global images of the Total Ozone Mapping Spectrometer (TOMS) aerosol index indicating the location of UV-absorbing tropospheric aerosols from July through September, 1988. Here, light brown indicates the smallest amount of dust/smoke in the atmosphere, with dark brown indicating the largest amount.
N
S
EW
![Page 11: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/11.jpg)
http://ingrid.ldgo.columbia.edu/maproom/.Global/.Climatologies/Precip_Loop.html
![Page 12: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/12.jpg)
Seasonal temperature variations can be explained in terms of the latitudinal and seasonal variations in the surface energy balance. The pattern of temperatures are a function of net short-wave radiation, net long-wave radiation, sensible heat flux, latent heat flux and change in heat storage.
http://geography.uoregon.edu/envchange/clim_animations/
![Page 13: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/13.jpg)
Precipitation-Evaporation (P-E) represents the difference between precipitation and evaporation
http://geography.uoregon.edu/envchange/clim_animations/
![Page 14: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/14.jpg)
Some implicationsAt 30°N/S latitudes, sea surface salinity tends to be high and deserts tend to cluster on land.When equatorial surface wind blows to the west, it also stacks the warm surface waters to the west, so producing the E—W temperature differential that produces the hurricanes and cyclones that strike eastern margins of tropical/semitropical land.
![Page 15: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/15.jpg)
http://www.scivis.nps.navy.mil/~braccio/images/S_big.gif
Sea Surface Salinity
![Page 16: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/16.jpg)
http://pubs.usgs.gov/gip/deserts/what/world.html
Deserts tend to cluster about 30º North and South latitudes, towards the western margins of land.
![Page 17: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/17.jpg)
Tropical cyclones develop in the hot, humid air over a sea surface exceeding 26°C in temperature.
![Page 18: That Climate Thing](https://reader036.vdocuments.net/reader036/viewer/2022062720/56813478550346895d9b58e6/html5/thumbnails/18.jpg)
Hurricanes typically occur on our Atlantic coast and originate
farther to the east, as can be seen in this animation of
Hurricane Katrina.