Desert Environments - PowerPoint PPT Presentation

1 / 18
About This Presentation
Title:

Desert Environments

Description:

May be influenced by rain shadow. Winter - high pressure region ... No rain since low volume and inversions prevents convectional rise. ... – PowerPoint PPT presentation

Number of Views:141
Avg rating:3.0/5.0
Slides: 19
Provided by: davidfi
Category:

less

Transcript and Presenter's Notes

Title: Desert Environments


1
Desert Environments
2
What is a desert?
  • Water - predominant controlling factor of
    biological processes.
  • Precipitation is highly variable
  • Variation in precipitation has a large
    unpredictable component.
  • Where precipitation 1/2 the potential
    evaporation.

3
Causes of deserts
  • Dry air dropping at 30Âş latitude
  • Cool coastal deserts (Baja, Atacoma of Chile
    Peru, Namib) add the cool coastal water.
  • Rain shadow effects

30Âş
0Âş
0Âş
30Âş
4
Physical factors insolation
  • Dry air and low, sparse vegetation - high of
    suns rays hit the ground directly.
  • Ground reradiates energy
  • Color of soil
  • Night radiation continues
  • Large fluctuations in temperature.

5
Subtropical deserts
  • Mediterranean climate
  • Cooler winter temperature
  • Typically at 300 - includes the Sahara, Arabian,
    Sonoran in the northern Hemisphere and the
    Australian, Kalahari (So. Africa) in the southern.

6
Subtropical deserts
  • Poleward boundaries of subtropical boundaries
    begin to blend with high deserts.
  • Polar air masses
  • Winter precipitation - summer drought
  • In No. Hemisphere, polar air masses may drop
    temperatures below freezing.

7
Continental Interior
  • Away from maritime influence. May be influenced
    by rain shadow.
  • Winter - high pressure region
  • Winter precipitation often as snow - from fronts.
  • Summer precipitation spotty and low.

8
Cool, Coastal Deserts
Atacoma
  • Similar locations to those of subtropical deserts
  • Often due to upwellings (15-18ÂşC).
  • Thin layer of air is affected by water
    (temperature inversion).
  • No rain since low volume and inversions prevents
    convectional rise.
  • Fog develops in 3 situations
  • At coast when temperature drops
  • 16-40 mi. inland nocturnally
  • Seaward Mtn. slopes

Atacoma
9
Heat transfer
10
Water Gain and Loss
  • Sources of water
  • Oxidation water
  • Food
  • Drinking Water
  • Loss of water
  • Evaporation from lungs
  • Evaporation from skin
  • Water in feces
  • Water in urine

11
Adaptations to Desert Environments
  • We will consider adaptations made by plants and
    animals to desert conditions such as
  • High light
  • High temperatures
  • Fluctuating temperatures (day/night)
  • Dry air - with somewhat random rain events
  • Dry soil
  • Lack of cover for protection from predators

12
Plant Adaptations
  • Three Major strategies
  • escape drought

High variability rainfall - annuals 96 of
flora Low variability rainfall - 1 of flora
13
Adaptations (cont)
  • evade drought

14
Adaptations (cont)
  • tolerate drought

15
Animal Adaptations
  • Escape heat drought
  • Aestivation
  • Diapause
  • Migration
  • Retreat

Fairy shrimp
Phainopepla
16
(No Transcript)
17
(No Transcript)
18
(No Transcript)
Write a Comment
User Comments (0)
About PowerShow.com