Weather And Climate Flashcards
Climate
The average weather conditions over a long period of time (20-30yrs). The climate is what we expect the weather to be like at a certain time based on the many years of observation
U.K. Climate type
Temperate maritime
T- moderate not the coldness of poles or heat of tropics
M- strongly influenced by the sea
Weather
The short term changes in the atmospheric conditions (precipitation, temp, wind)
U.K. Temp
Coldest in N England and Scotland
Warmest in S (w in winter and e in summer)
Coastal areas slightly warmer, hilly regions slightly colder
U.K. Precipitation
Driest in east
Wetter in west
Upland areas have more precipitation
U.K. Sunshine hrs
Sunniest in south and SE
Least sunny in north
Climate graph rules
Pattern of rainfall
Pattern of temp
Relationship
Anomalies
Temp climate graph
Overall shape
Highest temp (value and month)
Lowest temp (v and month)
Range
Rainfall climate graph
Seasonal differences Highest rainfall (v and month) Lowest rainfall (v and month) Range Total precipitation per year
Latitude uk (T)
Due to curvature of earth, sun’s rays at an oblique angle to the earth
Suns rats travelled through more atmosphere
Isolation spreads over a larger area
There fore less intense
Air pressure uk (R)
At equator air is warmed by high rate of solar insolation, density reduced so it rises
At about 30c it begins to sink and cool as density increases
At the same time, at the N pole air us sinking due to low pressures and it moves south until meeting warm air (60c) here warm air forced to rise creating low pressure
U.K. Is located here- frequent rainfall
Prevailing winds uk (T, R)
From south west
Wet from Atlantic
Mild due to warm ocean current
Distance from sea (T)
Continental effect
- large distance from sea
- land is poor insulator as it heats and cools quickly
- winters is cold, summer is hot
Maritime effect
- close to sea
- sea takes long time to heat and cool
- mild winters and cooler summers
Prevailing winds def
Wind from most frequent wind direction a location experiences
Altitude uk (T, R)
Temp decreases by 1 degree for every 100m
Because air density is reduced
Upland areas get more rain (relief rainfall) as air is forced to rise above them