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Atmos' Water Content

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Transpiration- water vapor that is given off by plants ... Sea Salt, Sand/dirt, Bugs, Pollen, etc. Anthropogenic CCN. Pollution Sources, etc. Cloud types ... – PowerPoint PPT presentation

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Title: Atmos' Water Content


1
Atmos. Water Content
  • Collect Hmwk 1, answers posted on Monday

2
Last Time
  • Hydrological Cycle
  • See diagram
  • Transpiration- water vapor that is given off by
    plants
  • Evapotranspiration- combines evaporation and
    transpiration effects
  • Numbers 97 of water resources tied up in oceans

3
Water Resources
  • 97 in Oceans
  • Fresh Water 0.09
  • In Atmos 1/1000th of a percent
  • A lot of importance though
  • Where do we find this small percentage in the
    atmosphere?

4
Water Vapor
  • Water vapor in the vertical
  • Since temp decreases with height (lapse rate 6.5
    deg C per km, 3.8 F per 1kft)
  • Therefore water vapor content decreases with
    height
  • mixing ratio drops off more dramatically with
    height than temperature
  • Above 850 mb, water content drops off rapidly
  • Most is contained between 1000-850 mb

5
Water Content (cont)
  • Where is the water mass on the earth?
  • See handouts given in classNCAR Tech Memo-
    Distribution of Topographical Quantities 1995
  • Winter cloud cover- in mid-latitudes over the
    oceans (both northern and southern hemisphere)
  • India and Sahara less cloudy regions in winter,
    some subtropical regions as well

6
Cloudiness (cont.)
  • In summer, in mid-latitudes over ocean is still
    cloudy
  • In summer the cloudiness in N.H. moves slightly
    northward
  • July-August low cloudiness, major deserts, Saudi
    Arabia, Australia, Sahara
  • Cloud cover over land 50

7
Page 1.40
  • Relative humidity with height ,averaged in
    latitudinal bands
  • Features are fairly similar in both winter and
    summer
  • Values greater than 70 represent the boundary
    layer, which makes sense
  • In the S.H. boundary layer is fairly moist from
    equator to pole, N.H dries out around 30 N.trade
    wind deserts

8
Function of land mass
  • Function of the land
  • N.H. 39 land, and 61 ocean
  • S.H. 19 land, and 81 ocean
  • Big land ocean dist asymmetry

9
RH x-y plots
  • Oceanic areas more humid, land masses are dry,
    except for the tropical rain forests
  • Siberia in the summer is relatively humid
  • SE US with humidity in the summer can be some of
    the most uncomfortable places in the world

10
Figure 1.43- PW
  • Precipitable Water (PW) The sum of the values of
    mixing ratio in a column of atmosphere
  • Lots of PW near the equator where it is warmest
  • In summer in N.H. high PW values reach the
    Southern US

11
Figure 1.45
  • Average precipitation over all longitudes for
    each latitude belt
  • High amounts are found in the equatorial regions,
    where it is warmest (among other
    processes---ITCZ)
  • Secondary maximums around 30 N and 30
    Smid-latitude jet streams are found here
  • X-Y plot is the final diagrammore handouts
    coming in the near future when we discuss gen
    circ further

12
Cloud Formation
  • Dr. Lupos 3-legged stool example
  • 3 things to get cloud
  • Moisture
  • Vertical motion (lift)
  • Cloud Condensation Nuclei (CCN)
  • Natural CCN
  • Sea Salt, Sand/dirt, Bugs, Pollen, etc.
  • Anthropogenic CCN
  • Pollution Sources, etc.

13
Cloud types
  • Cloudiness impacts temperature- cloudy nights
    warmer than clear, for example
  • High Clouds
  • Cirrus-type clouds, ice crystals
  • Middle Clouds
  • Alto, ice crystals and supercooled droplets
  • Low Clouds
  • Main Precip producersNimbostratus (uniform
    sheet) vs. Cumulonimbus (convective heap)

14
Precip Clouds (cont.)
  • In N.H. nimbostratus dominate in winter,
    cumulonimbus dominate in warmer seasons
  • Nimbostratus, are uniform with a large area of
    weak forcing, warm frontal (stratiform)
    precipitation
  • Cumulonimbus can grow up to 60000 feet, severe
    thunderstorms, heavy convective precipitation,
    high albedo only snow is higherclimate impacts

15
Drought
  • Places that are typically moist, but can become
    dry over a long duration, 2003 was a recent
    drought locally
  • 1988 was a widespread drought in the US
  • Different types of drought
  • Meteorological
  • Agricultural
  • Hydrological

16
Drought (cont.)
  • Basic drought equation precipitation minus
    evaporation
  • If evaporation exceeds precip for quite a time,
    the result is a drought
  • Meteorological drought compares P-E to climatology

17
Palmer Index
  • Rates a severity for drought
  • Long term indexcannot tell you if you have had
    relief due to a month being rainy
  • For more information
  • www.drought.noaa.gov/palmer.html
  • Also see the Drought Mitigation CenterUniversity
    of Nebraska-Lincoln
  • www.drought.unl.edu/whatis/indicies.htm
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