weather and climate Flashcards

1
Q

Air pressure

A

The weight of air on the Earth’s surface measured by a barometer in Millibars

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2
Q

Air Temperature

A

The degree or intensity of heat present in the atmosphere, measured by dry and wet thermometer and places in a Stevenson Screen

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3
Q

Cloud cover

A

The amount of clouds in a sky measured by observation in Oktas

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4
Q

Precipitation

A

Water falling from the sky in different forms, snow, sleet, hail, fog. Measured by a rain gauge in mm

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5
Q

Relative Humidity

A

The quantity of water vapor in parcel of air, measured by a hygrometer in grams of water vapor per kilogram of dry air

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6
Q

Wind speed

A

The velocity of moving air in the atmosphere, measured by an anemometer, usually in knots(nautical mile per hour

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7
Q

Wind direction

A

Measured from the direction wind comes from, measured by a wind vane

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8
Q

Isobars

A

lines on a weather map joining together places of equalatmospheric pressure

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9
Q

weather in low pressures

A

wet and windyweather

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10
Q

weather in high pressures

A

dry, sunny weather

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11
Q

Air pressure range

A

from900 mb(a hurricane) to1100 mb(an anticyclone).

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12
Q

isohyet

A

A line on a map that joins up places of equal rainfall

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13
Q

isotherm

A

A line on a map that joins up places of equal temperature

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14
Q

equatorial climate

A

Equatorial –heavy rainfall all year
Temperature - 25-30 all year, cold winters, mild summers
Annual rainfall – less than 250mm.

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15
Q

types of deserts

A

Extremely arid areas
Arid areas ( hot deserts)
Semi - arid areas
Cold deserts

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16
Q

extremely arid areas

A

have at least 12 consecutive months without rainfall e.g. Atacama desert.

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17
Q

Arid areas ( hot deserts)

A

less than 250mm of annual rainfall e.g. Namib desert.

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18
Q

Semi - arid areas

A

Less than 500mm of annual rainfall e.g. Mali

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19
Q

Cold deserts

A

Less than 250mm of rainfall. Located in interior of a continent or high latitude. Lower temperatures, often minus degrees in winter months.

20
Q

where are deserts located

A

near the Tropics of Cancer and Capricorn

21
Q

equatorial climate

A

home to TRF, heavy rainfall all year & temp 25-30 all year.

21
Q

arid climate

A

( tropical zone) – deserts, clear skies, cool night, day time temp can exceed 45. Low annual rainfall – less than 250mm.

22
Q

polar climate

A

cold ( below zero temp)and dry all year

23
Q

tundra climate ( sub polar)

A

located 60-70 degrees North, cold and dry, slow growing plants

24
Q

grasslands (subtropical zone)

A

Distinct wet & dry seasons – located 15-30 N/S.

25
Q

relief rainfall

A
  1. occurs when warm, moist air from the Atlantic Ocean rises up over mountains.
  2. When the warm air rises, it cools and condenses to form clouds, which brings rain.
  3. Once the air has passed over the mountains, it descends and warms.
  4. This creates drier conditions known as arain shadow
26
Q

conventional rainfall

A
  1. usually occurs during the summer in the UK, when the sun heats the land.
  2. This creates rising pockets of warm air, known as convection currents.
  3. Warm air rises rapidly, where it starts to cool and condenses to form clouds.
  4. These clouds can be largecumulonimbusclouds.
  5. The clouds can produce heavy rainfall and thunderstorms.
27
Q

latitude

A
  • distance from the equator
  • Temperatures drop the further an area is from the equator due to the curvature of the earth
28
Q

altitude

A
  • height above sea level
  • Locations at a higher altitude have colder temperatures. Temperature usually decreases by 1°C for every 100 metres in altitude.
29
Q

distance from sea

A

Oceans heat up and cool down much more slowly than land. This means that coastal locations tend to be cooler in summer and warmer in winter than places inland at the same latitude and altitude

30
Q

prevailing wind

A

The prevailing wind is the most frequent wind direction a location experiences

31
Q

climate in tropical rainforests (TRF)

A
  • Low pressure all year on the Equator.
  • Midday sun almost vertical, giving maximum isolation.
  • Average temperature all year round 26 degrees Celsius.
  • Heavy convection rainfall and thunderstorms in the afternoon, as the sun has warmed the ground, causing the air to rise.
  • Average annual rainfall 1750 - 2500mm
  • High relative humidity 75%.
32
Q

soil in TRF

A
  • Most of the soil is not veryfertile.
  • A thin layer of fertile soil is found at the surface where the dead leaves decompose.
  • It is red in colour because it is rich in iron.
  • Due to heavy rainfall the nutrients are quickly washed out of the soil.
33
Q

lianas

A

these are woody vines that have roots in the ground but climb up the trees to reach the sunlight. Their leaves and flowers grow in thecanopy.

34
Q

tree trunks

A

these are tall and thin to allow trees to reach the sunlight. The bark on these trees is smooth to allow water to flow down to the roots easily

35
Q

drip tips

A

plants have leaves with pointy tips. This allows water to run off the leaves quickly without damaging or breaking them.

36
Q

epiphytes

A

these are plants which live on the branches of trees high up in thecanopy. They get their nutrients from the air and water, not from the soil.

37
Q

buttress roots

A

large roots have ridges which create a large surface area that help to support large trees.

38
Q

animal adaptations in TRF

A
  • Theslothusescamouflageand moves very slowly to make it difficult forpredatorsto spot.
  • Thespider monkeyhas long, strong limbs to help it to climb through the rainforest trees.
  • Theflying froghas fully webbed hands and feet, and a flap of loose skin that stretches between its limbs, which allows it to glide from plant to plant.
39
Q

characteristics of hot deserts

A
  • Hot seasons for most of the year
  • Average monthly temperature of 29 degrees Celsius.
  • Average annual rainfall of less then 250mm
  • Temperature range of 5-50 degrees Celsius.
  • Low humidity 25-30%
  • Clear skies all day and night
  • Coarse sandy soils with good drainage, little sub-surface water, low in nutrients and organic matter.
40
Q

causes of hot deserts

A
  • hight pressure
  • cold ocean currents
  • rainshadow effect
  • continentality
41
Q

high pressure

A
  • sinking air warms and dries by compression
  • no clouds = no rain
42
Q

low pressure

A

deep rain cloud

43
Q

cold ocean currents

A

ensures that there is little moisture available to cool and form clouds

44
Q

rainshadow and continentality

A

Air descending from mountainous areas warms and dries by compression, little rainfall forms and aridity is the result.