Weather is defined as the state of the atmosphere at a specific point in time.
Parameters to describe weather include:
Temperature
Precipitation
Humidity
Wind speed
Cloudiness
Sunlight intensity
Convection
Convection: Heat transfer due to bulk movement of molecules within fluids (gases, liquids).
Emerges from fluids warmed from below.
Rising parcels of fluid cool at higher elevations.
An efficient way to transfer heat.
Essential for storm formation, ocean circulation, and plate tectonics.
Thunderstorms
Thunderstorms develop from atmospheric convection:
Warm, moist air rises, cools, and condenses releasing heat.
Further cooling can lead to freezing, releasing additional heat.
Storms organize into intense circulation; precipitation occurs as condensed water rains out.
Can persist as long as warm, moist air is available.
Tropical Weather
Characterized by two main seasons:
Wet Season: Dominated by convection and thunderstorms.
Dry Season
Key weather systems include:
Inter-Tropical Convergence Zone (ITCZ)
Monsoons
Tropical Cyclones
Inter-Tropical Convergence Zone (ITCZ)
A band of thunderstorms encircling the Earth, forming where the sun is overhead.
Position influences local rainfall patterns:
Shifts north and south with seasons (farthest north during Northern Hemisphere summer, and vice versa).
Affects mid-tropics with two rainy seasons; surrounding regions receive one.
Monsoons
Caused by land-sea temperature differences:
Heating of land creates a low-pressure zone, drawing in moist ocean air.
Enhanced by geographical features (e.g., mountain ranges).
Cycle reverses in winter, leading to dry conditions.
Tropical Cyclones
Form from clusters of thunderstorms in warm sea conditions (>26°C).
Requires:
Warm ocean water
Low shear winds
Ability to organize into a low-pressure system.
Naming conventions vary by region:
Hurricanes: Atlantic, Eastern Pacific
Typhoons: Western Pacific
Cyclones: Indian Ocean
Extra-Tropical Weather
Dominated by high and low-pressure systems:
High pressure from descending winds; low pressure from rising air.
Air movement creates pressure gradients influencing weather patterns.
High pressure typically leads to clear, sunny weather; low pressure results in cloudiness and storms.
Front Formation
Fronts are boundaries between air masses:
Warm Fronts: Warm air rises over cooler air, leading to gradual temperature increases and light rain.
Cold Fronts: Cold air forces warm air upwards, resulting in heavy precipitation and strong winds.
Occluded Fronts: Form when a cold front overtakes a warm front, lifting warm air to create intense precipitation.
Extreme Weather
Defined as unexpected, unpredictable, severe, or unseasonal weather.
Includes storms (tropical cyclones, tornadoes) and extreme temperature events (heat waves, cold waves).
Tornado Formation
Developed through:
Shear winds creating horizontally rotating air.
Updrafts catching spinning air and bending it vertical.
Formation of a super-cell thunderstorm capable of producing tornadoes.
Tornadoes are short-lived yet can be extremely intense; capable of causing localized severe damage.
Local Weather Effects
Local geographical features also influence weather:
Orographic Precipitation: Moist air rises over mountains, cools, and precipitates, leaving a dry rain shadow on the leeward side.
Sea Breezes: Generated by temperature contrasts between land and ocean, moving air from ocean to land.
Katabatic Winds: Cold, dense air flowing downhill from high elevations; strongest in valleys and over glaciers. These winds can reach over 300 ext{ km/h}.