Rnr Deserts

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25 Terms

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Coastal Deserts

usually occur on western continental edges and are affected by cold coastal currents that inhibit rainfall to adjacent land masses, although morning fogs provide water to a relatively high diversity of plants and invertebrates

<p>usually occur on western continental edges and are affected by cold coastal currents that inhibit rainfall to adjacent land masses, although morning fogs provide water to a relatively high diversity of plants and invertebrates</p>
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Hadley Cell Circulation

The model that explains global air circulation and precipitation patterns according to latitudinal differences.

<p>The model that explains global air circulation and precipitation patterns according to latitudinal differences.</p>
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Coreolis effect

The effect of Earth's rotation on the direction of winds and currents.

<p>The effect of Earth's rotation on the direction of winds and currents.</p>
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Mid-latitude deserts

are poleward of the Trade Wind Deserts, and are impacted by dry Westerly air currents moving towards the Polar Cell. Are classified as "cold" deserts, with winter. temperatures often below 10 C

. Taklamakan Desert in southcentral China

. Great Basin in the western U.S.

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Monsoon Deserts

are caused by seasonal wind shifts, e.g., the Rajasthan Desert in western India, which receives dry air from the Himalayas and Siberia during the winter, but moist air from the ocean during summer heating (rising air)

<p>are caused by seasonal wind shifts, e.g., the Rajasthan Desert in western India, which receives dry air from the Himalayas and Siberia during the winter, but moist air from the ocean during summer heating (rising air)</p>
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Examples of morphological and physiological adaptations that plants have created in order to live in the desert

. smaller leaves

. sunken stomata that only opens at night to reduce water loss

. spines are to help protect itself from harm, but ALSO to provide shade for plants

. rolled leaves trap moist air above

. hair on lower leaf to trap moisture

. dormancy leaf incision

. desiccation-resistant seeds in deserts

. extensive shallow root systems for rapid water uptake after rainfall (cactus), or deep roots (phreatophytes) to access deeper water sources (60 m in mesquite trees)

. They have large diameter xylem for transferring large amounts of water from the ground to the canopy, and often lose considerable water to transpiration

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Examples of Behavioral and Physiological adaptations that animals have created in order to live in the desert

. Dew collection on scales

. Big radiative ears to help them cool down

. Fat/water storage

. Uric acid secretion

. Salt excretion

. Burrowing

. Crepuscular/nocturnal activity periods

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- Thorny Devil

- Namib desert beetle

Dew collection on scales: animal example

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- Jackrabbit

- Fennec Fox

Radiative ears: animal example

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- Gila Monster

- Camel

Fat/water storage: animal example

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Dorcas Gazelle

Uric acid secretion: animal example

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Roadrunner

Salt excretion: animal example

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- desert skinks

- Desert Toad

- Desert Tortoise (escape heat)

- Horned Lizard (access heat at night)

Burrowing: animal example

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-Kangaroo Rat

-Rattlesnake

-scorpions

- geckos

- owls

Crepuscular/nocturnal activity periods: animal example

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closable nostrils, ear hairs, eyelashes, and nictitating membrane to protect their eyes from sand

What do camels have that helped them adapt to their environment?

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Phreatophytes

are plants that have become adapted to arid and semi-arid ecosystems by developing extensive root systems that extend to the water table

<p>are plants that have become adapted to arid and semi-arid ecosystems by developing extensive root systems that extend to the water table</p>
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Phreatic zone

saturated zone below the water table

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Polar Deserts

Cold, dry areas of high pressure at the poles. Occur in areas where precipitation averages <25 cm and mean temperatures during the warmest month is <10 C. Antarctica's Dry Valley has been ice-free for thousands of years.

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Rain shadow deserts

Desert formed on the leeward side of a mountain range because the height of the mountain prevents most moisture from crossing over it

<p>Desert formed on the leeward side of a mountain range because the height of the mountain prevents most moisture from crossing over it</p>
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Sclerophyllous plants

a type of vegetation that has hard leaves, short internodes and leaf orientation parallel or oblique to direct sunlight.

<p>a type of vegetation that has hard leaves, short internodes and leaf orientation parallel or oblique to direct sunlight.</p>
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Trade Winds deserts

are impacted by dry air currents (descending Hadley Cell circulation) moving towards the equator, which dissipate clouds (absorb water) and maximize incoming solar radiation. Temperatures in the Sahara have been recorded at 57 C (135 F)

<p>are impacted by dry air currents (descending Hadley Cell circulation) moving towards the equator, which dissipate clouds (absorb water) and maximize incoming solar radiation. Temperatures in the Sahara have been recorded at 57 C (135 F)</p>
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Xerophytes

plants with adaptations that enable them to survive in dry habitats or habitats where water is in short supply in the environment.

- Cacti

- Prickly pear

- Bromeliads

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Soil salinitization

occurs when water soluble salts, such as NaSO4, CaSO4, or MgSO4, accumulate in the soil. Water seeping from the soil evaporates, leaving the salts behind. Making it harder for plants to absorb water in salty soil

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Hydrenchyma

special water storage tissue with elastic cell walls that can swell when water is abundant, and collapse during dry periods as the plant uses the stored water.

<p>special water storage tissue with elastic cell walls that can swell when water is abundant, and collapse during dry periods as the plant uses the stored water.</p>
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Transpirational loss

Water loss through evaporation from plant surfaces.