INDEPENDENT STUDY
Air masses
Fronts
Winds
Breezes
Are large bodies of air that have similar traits, such as humidity, temperature and air pressure throughout
4 Types of Air Masses:
Continental
Polar
Tropical
Maritime
Form over land, and as a result are very dry due to the lack of moisture over land
Very moist, due to forming over oceans
Very hot and warm, due to forming in hot regions
Very cold, due to forming in colder regions
Transition periods where air masses meet but don't mix
These Air masses can combine to form new ones, for example, Tropical Continental
Yet again, there are 4 types of fronts
Cold Fronts
Occluded Fronts
Warm Fronts
Stationary Fronts
Where warm air replaces cold air
Cold air replaces warm air. These form faster than most other fronts
When warm and cold air are at a standstill, where neither one can move
When warm air is caught between 2 cold air masses
All of the topics mentioned here are caused by Convection! Convection is where warm air rises while cold air sinks. This is also the transfer of heat through fluids
Continental Tropical
Maritime Tropical
Maritime Polar
Continental Polar
Dry and cold winds
Wet and Cold winds
Dry and hot winds
Wet and hot winds
A cold front occurs when a rapidly moving cold air mass and a slowly moving warm air mass meet. The warm air mass rises, cools, and condenses, often bringing precipitation.
Warm fronts occur when a fast-moving warm air mass meets a slowly-moving cold air mass. If the warm air is humid then rain. if the warm air is dry then scattered clouds.
Thunderstorms form within large cumulonimbus clouds. Most cumulonimbus clouds form when warm air is forced upward at a cold front.
Where the warm and cool air meet, water vapor in the warm air condenses into rain, snow, fog, or clouds. If the front stays stalled over one area, it could bring many day of clouds, and rain.
The denser cool air masses move under the less dense warm air masses and pushes it upward, the cooler air masses meet in the middle, and they may mix.
Flow from places of high pressure to places of lower pressure
A High Pressure system is an area of higher atmospheric pressure, accompanied by anticyclonic and outward wind flow.
A low pressure system is an area of lower atmospheric pressure, accompanied by cyclonic, inward flow.
These form because of downward motion in the atmosphere. Think of it as air just piling up in one spot. Now you have a big bubble of air pressing down and out on the Earth's surface.
These high pressure systems typically bring sunny, dry weather and calm winds. A lot of deserts are formed by permanent or semi-permanent high pressure systems.
Low pressure systems typically bring cloudy skies and some form of precipitation. Tropical cyclones and big snowstorms are all examples of low pressure systems.
Low pressure systems form from rising air and wind divergence in the upper levels of the atmosphere. So while air continues to rise up, it's also moving outward way up in the atmosphere, causing the amount of air in one spot to continually decrease.
This process is called cyclogenesis
Created when air flows from areas of higher pressure to areas of lower pressure, to reach equilibrium.
Warm air, which has less air pressure
Cold air, which has more air pressure
Meterologist: a scientist who studies the causes of weather and tries to predict it.
Wind is measured through 2 tools:
An Anemometer, which tells wind speed
A Wind Vane, which tells the direction in which the wind is flowing
2 types of breezes:
Like winds, they are still caused due to uneven heating of our atmosphere but travel a much shorter distance
Land Breezes
Sea Breezes
Note: Breezes are always named after WHERE THEY CAME FROM
Originated from land, only during the night where the air travels from the land to the sea. Warm air rises above the ocean, while cold air sinks over land
Originated from the sea, occurs only during the daytime where the air travels from the sea to land. Cold air sinks over the ocean while warm air rises above land
3 Types of Heat Transfer
Conduction: The heat transfer of solids
Radiation: Transfers through electromagnetic radiation
Warm air also holds more moisture than cold air
As it rises, the warm air containing the water vapor continues to cool. If it continues to cool, then it will reach a state called "supersaturation" in which some of the water vapor changes states to a liquid or solid. After this, the water in the atmosphere become visible, thus making a CLOUD
Types of Clouds and their descriptions, and the storms that may follow
Fog
Cumulus clouds
Cirrus clouds
Cumulonimbus clouds
Stratus clouds
Very thin, and they form incredibly high in the atmosphere
Usually resembling a low stratus, fog is a cloud near the ground
Tall, fluffy and white. They are flat at the bottom and usually is a sign that there is good weather on the way.
Long, thin blankets of gray clouds that usually mean decent weather, but they do make it gloomy.
Taller and darker versions of Cumulus clouds, which usually are a sign for heavy rain.
Extreme Weather
There are 3 main types of storms
Thunderstorms
Tornados
Hurricanes
a violent disturbance in the atmosphere, including thunder and lightning
a funnelling cloud that touches the ground on earth.
Turns out, convection causes all of these storms!
Clouds are the basis of thunderstorms, and clouds are formed due to warm air containing water vapor rising. Tornadoes gain their ferocious destruction and power through warm air circling around the funnel, while cold air goes down the middle. Unlike the tornado, for the hurricane cold air circles around the body while warm air fuels up the middle.
a tropical storm with winds that have reached a constant speed of 74 miles per hour or more
Stratus means "Layer"!
Cirrus means "Higher up"
Nimbo/Nimbus means "Precipitation"
Global Winds
3 Kinds of cells
Ferrrel Cells, when warm air rises and cold air sinks at 60 degrees north and south
Polar Cells, when warm air rises and cold air sinks at 90 degrees north and south
Hadley Cells, when warm air rises and cold air sinks at 30 degrees north and south
Coriolis effect: Due to the Earth’s rotation, winds and currents deflect to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
Trade Winds:They blow to the Southeast in the South and Northeast in the North. Winds that blow from 30 degrees latitude almost to the equator are called trade winds.
Polar Easterlies:They are formed as cold sinking air moves from the poles towards 60 degrees North and South Latitude.
Westerlies: They flow towards the poles from West to East. They can carry moist air over the Unites States producing rain and snow.
(Between 30 degrees latitude and 60 degrees latitude)
Uneven heating of the Earth produces pressure belt, and it occurs at about 30 degrees of latitude. The combination of Convection Belts and Coriolis Effect causes Global Winds Pattern.
Doldrums:There are regions that are CALM AREAS near the equator that do not have any wind or very little wind, as warm air rises. Near the equator there is little wind, so there is a lot of horizontal motion, and lots of precipitation.
Horse latitudes are CALM AREAS of sinking cold air and have very little precipitation and have calm winds (30 degrees North and South)
Winds blow steadily from specific directions over long distances. They are created by unequal heating of Earth’s surface
Global convection currents: These giant currents occur in the atmosphere and are produced by temperature differences between the equator and the poles.
Ocean and Surface Currents
Surface currents flow at or near the surface of the ocean & are driven by atmospheric conditions (winds).
Ocean Currents are the movement of seawater driven by gravity, wind, The Coriolis Effect and Water Density
An Upwelling is when surface winds displace the warmer surface water in the ocean.
The Global conveyor belt starts in the Arctic where sea water freezes without salt, so the salinity of the water around the ice increases, and it sinks, so warm water comes to take its place.
Salinity: The amount of salt in an object or thing
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El Niño:
La Nina
Occurs every 2-7 years, leads to weaker trade winds traveling in the opposite direction with more evapoartion and moisture in the atmosphere
Stronger Trade winds than usual, a cooling of the water in the Pacific Ocean followed by a global climate shift which brings stronger upwellings and a variation of preciptation in some areas.
As warm water from the equator moves towards the poles, it gets colder, and has a higher concentration of salt, because ice crystals that form trap water and leave salt behind. This cold, salty water sinks, and warmer surface water takes its place. This cold, salty water is now at the bottom of the ocean floor, and can only move in one direction: Horizontally. It sometimes rises again near the equator through upwelling, bringing nutrients to the surface. This warm water now moves towards the poles, cools down, gets saltier, and
ThermoHaline Circulation
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Ocean currents act much like a conveyer belt, transporting warm water from the equator toward the poles and cold water from the poles back to the tropics. Thus, currents help to counteract the uneven distribution of solar radiation reaching Earth's surface.
Water Troubles
Humans need Fresh Water to survive, but it only makes up about 3% of all water on earth
Salt water makes up the remaining 97%, but it is undrinkable without proper filtration
Of this 3%, 69% of it is underground, with 30% being frozen. So, around only .03% of all fresh water is actually drinkable
We are already affecting access to fresh water in many ways, like pollution. Pollution can lead to higher risks of devastating droughts, which affect dehydration, starvation which hurt biodiversity.
Around the world, about 125,000 species live in fresh water habitats, while millions of other species, like us require fresh water to drink
Losses in biodiversity can also lead to problems with the availability of food and a disruption of the food chain. This can lead to certain animals increasing or decreasing in mass, and could make some species invasive.
Biodiversity plays an important role in the cleaning of water. When water passes through most rivers and streams, they encounter a number of alage and fungi that filtrate the water so we can drink it.
Cloud Forests are a unique and valuable source of filtrated and clean water, due to being located in the clouds on the slopes of mountains.
Water condenses on the leaves of plants, leading to a constant drip of water flowing into streams, which makes clean, unpolluted water.
Also known as "water tamers" 💀 due to providing water for hundreds of nearby towns
They house an impressive and stunning array of plants and animals, despite only making up around 2.5% of all forests.
This is because they are incredibly fragile, and unable to recover from most forms of damage or pollution. It is estimated that 1.1% of all cloud forests are cleared out every year.
This has led to a GLOBAL WATER SHORTAGE.
Around 66% of a billion people remain without access to fresh water
Also called severe water scarcity, referring to when consumption is twice as high than available resources. This usually occurs in rural areas.
The consequences of water scarcity can lead to economical and food production losses.