Intro (Tropical Storms) Flashcards

1
Q
  • Within 5° of latitude north or south of the equator, no storms: Coriolis effect, weak
  • South Atlantic Ocean or in the Eastern part of the SouthPacific Ocean: cold ocean temperatures and persistent large wind shear
A

Tropical storms … formation

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2
Q
  • dissipate when traveling over cool water or over land

In these environments:
* source of hot humid air is lost
* over land, weaken fast, … no evaporation of warm ocean water

A

Tropical storms … death

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3
Q

the __________ known as the mid-latitudes and provide their approximate latitudinal range.

  • Mid-latitudes (30-60°N, 30-60°S)
  • Western coastal areas are wetter than their eastern
    counterparts.
  • Those remote from the ocean are drier.
  • Increasing latitude: lower mean surface temperature
A

geographical region

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4
Q

Greater temperature fluctuations within continental interiors compared with those near oceans.

A

Continentality

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5
Q

Mid-latitude Climates. West coast climates of lower latitude (nearer equator):

greater seasonality in their ________ than those nearer the poles

A

rainfall patterns

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6
Q

The ______ ______ sweeps
precipitating extratropical cyclones
from the Atlantic and Pacific oceans (where they are formed throughout the year due to the polar front)

A

westerly airflow

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7
Q

Wet weather of the western coast: due to prevailing __________ ___________

A

westerly airflow

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8
Q

West coast areas at the equatorial end of the mid latitudes (about 30°N) tend to have dry warm to hot summer and wet, cool winters.

A

mediterranean climate

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9
Q

Poleward of the mediterranean climate:

A

Marine west coast climates

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10
Q

Mid-latitude Climates

Eastern part is Influenced by___ _____ ______________

A

air mass movement

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11
Q

allow the boundary between these air masses to pass over much of this part  Climate: rapid and substantial fluctuations in
temperature

A

Fluctuations in Rossby waves

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12
Q

bathed in moist maritime and continental air

A

East coast of Asia

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13
Q

Frequent dry, essentially north-westerly winds to flow over the surface of the

A

eastern part of the mid-latitude
Asia

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14
Q

The wind flow is reversed in the summer months, bringing moist maritime winds and greater rain.

A

Eurasian interior

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15
Q

During winter, sustained large-scale high-pressure feature forms over Eurasian interior (centered over Mongolia).

A

Eurasian interior

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16
Q

Mid-latitude Climates

_________________
* Essentially same climatic influences as those in the north.
* But the land masses in the southern hemisphere are much less extensive than the northern counterparts.
* continental interior and east coast are less well developed
* South America: same as North American climates (except the lee of Andes mountains).

A

Southern hemisphere

17
Q

Climate Zones of the World: Arctic ( two seasons)

A

polar day and polar night.

18
Q

Climate Zones of the World: Mid-latitudes (four seasons)

A

summer, autumn, winter, and spring

19
Q

Climate Zones of the World: Tropics (two seasons)

A

wet and dry

20
Q

Polar Region (60-90°N, 60-90°S)
Cold
Warmest month: temperature ____

A

≤ 10 °C

21
Q

Much of the ground is permanently frozen

A

permafrost

22
Q
  • Low levels of precipitation is due to the low moisture carrying capacity of cold air and the stable atmospheric conditions found in the areas covered by the polar cell.
  • Despite the aridity, much of the land is covered with surface water (generally frozen).
  • Losses by evaporation and infiltration through the permafrost are low.
A

Frequently arid

23
Q

Polar Climate

Interior of the northern polar region:

A

Generally calm

24
Q

Polar Climate

Interior of the south polar region:

A

Blustery, strong winds of topographic origin are common
over the mountainous continent of Antartica.

25
Q
  • mechanisms mediating climate change, not fully understood
  • but, possible to build climate models (both predictive and interpretive value)
  • product of various components of the climate system
  • feedback mechanism
A

The Climate System