Weather: day-to-daycharacteristics of temperature, rain, cloudcover, and wind.
Climate: long-termweatherpatterns
Six major factors that determine the climate that exists in any particular location: Latitude, ocean currents, wind, elevation, relief, and nearness to water.
Latitude: the distancenorth and south from the equator
Latitude determines if a region is hot or cold
Ocean currents: bring warm or cold water to new places
Air Mass: Largevolume of air that takes on the climacticconditions of the areas in which it forms.
Elevation: refers to the height above sealevel.
The higher up you are the colder it feels, As air rises, the pressure decreases = air expands/cools
Relief: refers to the shape of the surface
of the land (high/low)
natural vegetation: the plants that would grow in an area with no human interface
dry climate soils: soils that develop where calcification is the dominant soil-forming process
wet climate soils: soils that develop where leaching is the dominant soil-forming process
soil profile: the three different layers that exist in the soil beneath the surface of the ground. Each layer has a particularcombination of physical, biological, an chemical characteristics.
annual temperature range: temperature of the warmest month subtracted from the coldest month
continental climate: climate in areas far away from bodies of water. Extremetemperatures and lowprecipitation <1000mm
Maritime climate: Climate in areas near large bodies of water. Mild winter/cool summers and high precipitation >1000mm
weather vs Climate: Weather is the day-to-day characteristics of temperature, rain, cloud cover, and wind while climate is the long-term weather patterns
if the ocean current is warm, it will heat the air; if it is cool then it will cool the air above
wind moves hot and cold "airmasses" to other places
if there was no wind the weather would not change
air moves from areas of high pressure to areas of low pressure ( moving air = wind)
Wind belts: well-established patterns of low and high pressure areas
mountains act like a barrier to air masses
nearness to water: regions that are close to oceans and large lakes have different climate
in the summer water remains cooler than the land and when the wind blows, it brings cool air over the land.
in the winter water keeps its heat and when wind blows, it brings warm air over the land.
Topsoil: dark thick layer. Large quantity of nutrient-rich organic material.
subsoil: less fertile and contains less organic matter. Harder and more compact
parent material: starting point for most soil development. maybe mineral rock or organic material
calcification: when there is a dry climate, water-carrying dissolved minerals move upwards toward the soil. Water evaporated leaving behind mineral deposits
leaching: during a wet climate, water from excess rainfall moves downward through the soil removing all minerals.
Tundra: - second largest vegetation
Tundra
second largest vegetation region
located in Canada'sartic
the surface is permanentlyfrozen-permafrost
treeless because of lowsummertemperatures and shortgrowingseason
soil has lowlevel of nutrients
Boreal and Taiga:
largest vegetation region
dominated by a sparely populated community of plants that survive cool short summers and long cold winters
most common coniferous trees. Evergreen is very shallow.
region is poorly drained
biggertrees more common in southern region eg. deciduous.
Mixed Forests:
has both coniferous and deciduous
pine and spruce are found in the same area as maple and oak.
transition zone
located southern East Canada like southern Ontario and quebec
has abundant and regular precipitation
humus from leaves creates fertile soil suitable for farming
Deciduous Forest:
located in southwestern Ontario
northern limit to many deciduous tree species
The area has been cleared for farming; only patches are left
hot summers, mildwinters, and precipitation occur throughout the year.