Weather Hazards Flashcards
(41 cards)
Polar insolation
Over large surface area of Earth, ‘Albedo effect’
Albedo effect
Sun’s rays are reflected off white snow/ice in poles
Equatorial Insolation
Over small surface area of Earth
Equator
0º on lines of latitude
Tropic of Cancer
23.5ºN on lines of latitude
Tropic of Capricorn
23.5ºS on lines of latitude
Artic Circle
66.5ºN on lines of latitude
Antarctic Circle
66.5ºS on lines of latitude
Wind
Air that moves from high to low pressure, Coriolis effect, Northern hemisphere forces winds to curve to right, so winds will blow clockwise, Southern hemisphere forces winds to curve to left, so winds will blow anticlockwise
Coriolis effect
Winds don’t blow in straight line as Earth is rotating
Weather in UK
Cloudy + wet as UK is in boundary of Ferrel + Polar cells + as there is low pressure from rising air
Low pressure
Where hot air rises, so weather is cloudy + rainy
High pressure
Where cold air sinks, so sky is clear + there is dry + clam weather
Weather in desert
Hot + dry due to high pressure, so there is lack of rainfall + clouds, lack of clouds makes it very hot during day, but very cold at night as heat is lost from ground, lack of rainfall makes it desert
Equator weather
Hot + humid due to low pressure, making weather very wet + cloudy, air rises due to equatorial insolation heats up air, making it rise + very hot
Hadley cell
It’s largest cell
Ferrel cell
Travels in opposite way to polar or hadley cells
Tropical storm
Huge storm that forms + develops in Tropics, USA + Caribbean - hurricanes, Japan + Philippines - typhoons, Australia + South-east Asia - cyclones, form above 27ºC
Extreme weather
When weather event is significantly different from average/usual weather pattern + it’s especially severe or unseasonal
Global Atmospheric Circulation
Movement of air + heat across Earth, creates areas of high rainfall e.g tropical rainforests + areas of dryness e.g deserts,
Distribution of Tropical Storms
Form 5-15º North or South of Equator (in Tropics) as they need water to be 27ºC or hotter to form, majority form in Northern Hemisphere
Formation of a Tropical Storm
Strong upward movement of air draws water vapour up from warm ocean surface, this evaporated air cools as it rises + condenses to form towering thunderstorm clouds, as air condenses, it releases heat which powers storm + draws up more + more water from ocean, several smaller thunderstorms join together to from giant spinning storm, now develops eye +, therefore, eye wall too, as storm is carried across ocean by prevailing winds, it continues to gather strength, on reaching land, storm’s energy supply is cut off, friction with land slows it down + it begins to weaken, if storm reaches warms seas after crossing land, it may pick up strength again
Eye
Centre of storm, where air descends rapidly
Eyewall
Outer edge of eye, where most intense weather conditions are felt