Lecture 8 Flashcards

1
Q

The pressure difference between the Icelandic low and Bermuda high is important to?

A

European severity

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2
Q

What’s the zone where trade winds converge?

A

Inter-tropical convergence zone (ITCZ)

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3
Q

Monsoon climate

A

Refers to the reversal of mean surface wind direction from summer to winter

Most regions between 35 N + 25 S and between 30 W + 170 E experience monsoon climate (best known in S + SE Asia)

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4
Q

What is responsible for the relatively mild climates of western and Northern Europe?

A

The North Atlantic Current (the ‘Gulf stream’)

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5
Q

What is the influence of the Himalayas?

A

They cast an extensive rain shadow comprising the Tibetan Plateu + the Taklamakan desert

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6
Q

What are the 7 factors that determine climate?

A

Latitude - determines how much average solar radiation a given location receives, which impacts seasonality
Land and water - determines continentality of a given location
Ocean currents - can provide e.g. An additional heat source for a region
Prevailing winds - determine e.g. How much moisture is advected + hence determine potential for rainfall
Pressure cells - determine availability of cloud coverage and frontal systems
Mountain barriers - can deflect wind or result in rain shadow on the leeward side
Altitude - has an influence on temperature

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7
Q

What is climate?

A

Long term averages of weather conditions and the range of variability with respect to the mean value

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8
Q

What is Weather?

A

Described through temperature, pressure, rainfall, visibility and cloud coverage

Current physical state of the atmosphere

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9
Q

What are the two systems of climate classification?

A

Thornthwaite - based on moisture (soil and ET), used mainly by scientists
Koppen system - based on temperature and precipitation, linked to vegetation (tropical moist, dry, moist-mid latitude with severe/mild winters, polar climates)

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10
Q

What largely determines average wind and pressure distribution?

A

Semi-permanent highs and lows

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11
Q

What causes climate variability?

A

Caused by natural changes in climate that fall within the normal range of extremes for a particular region
Measured by: temperature, precipitation and frequency of events
Atmospheric oscillations = important driver for natural climate variability

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12
Q

What is the positive phase of the North Atlantic oscillation?

A

Stronger than usual pressure difference.

Fast storm tracks bring wet warm winters in W.Europe, mild and wet winters on N. American East Coast

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13
Q

What is the negative phase of the North Atlantic oscillation?

A

Weaker pressure difference

More cold air invasions on N. American East Coast and in Mediterranean Europe

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14
Q

What is the North Atlantic oscillation?

A

Defined as the difference between sea level pressure between 2 stations during the winter season (dec-mar)

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15
Q

What two pressure cells are involved in the North Atlantic oscillation ?

A

Icelandic low pressure cell

Azores-Bermuda high pressure cell

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16
Q

Name the environmental spheres?

A

Lithosphere, biosphere, hydrosphere, atmosphere

17
Q

The environmental spheres of the earth/climate system interact through feedbacks, what are they and what do they cause?

A

Positive - instability, change accelerates

Negative - stability, change slows down

18
Q

The strength of a feedback on temperature is called ?

A

Feedback factor and is defined:

F = (temperature change with feedback)/ (temperature change without feedback)

If F has the value of 1, no feedback exists

19
Q

Why should we be bothered about climate change?

A

Environmental problems and harm it may bring
Our way of life is fairly dependent on certain range of climatic conditions, even though technological advancements have slightly reduced this independence
Effects ecological processes and ecosystems
Natural climate variability (e.g. El Niño/droughts) causes economic loss and suffering

20
Q

What natural variability influences the global average surface temperature?

A
Changes in incoming solar radiation (orbital changes, solar outputs)
Continental drift (affects thermohaline circulation, rate of chemical weathering) 
Changes in earths albedo (volcanic winter, polar ice caps)
Changes in outgoing terrestrial radiation (increased GHG effect)
21
Q

Milankovitch cycle

A

3 most common orbital changes
Changes in eccentricity - varies 100,000yrs
Variations in obliquity - between 21.6 + 24.5 degrees, over 41,000yrs
Changes in precession and point of perihelion - 23,000yrs
Currently the earth is closest to the sun in January - in 11,000yrs the perihelion point = July

22
Q

Ice core records at 3500m depth show…

A

Atmospheric records dating back almost 700,000 years BP