Physical Geography Climate and Vegetation Climate is created by the sun’s solar energy interacting with the earth’s land, water, and air. In turn, climate.

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Presentation transcript:

Physical Geography Climate and Vegetation Climate is created by the sun’s solar energy interacting with the earth’s land, water, and air. In turn, climate and soil shape the earth’s vegetation. Street sweepers in New Delhi, India, take a break amid floodwaters from July 2003 monsoon rains. NEXT

Section 1 Seasons and Weather 9 slides

Seasons Seasons and Weather SECTION 1 NEXT Earth’s Tilt Earth is tilted at a 23.5° angle relative to the sun Areas of Earth get more, less direct sun at different times of year The seasons are related to the earth’s tilt and revolution

The solstice marks beginning of summer, winter -sun’s rays directly overhead at noon at furthest points north and south The equinox marks the beginning of spring and autumn -day and night are equal in length

Weather Weather and Climate Weather—atmospheric conditions at a particular location and time Climate—weather conditions at one location over long a period Example: Northern Russia has a cold climate SECTION 1 NEXT Continued...

What Causes the Weather? Sun: amount of solar energy received Water vapor: determines whether there will be precipitation Precipitation—water droplets falling as rain, snow, sleet, hail Cloud cover: clouds may hold water vapor

SECTION 1 NEXT What Causes the Weather? Landforms and bodies of water -water heats slowly, loses heat slowly -land heats rapidly, loses heat rapidly Elevation: as elevation increases, air becomes thinner -thin air cannot hold moisture Air movement: distributes moisture and solar energy continued Weather Continued...

SECTION 1 NEXT Precipitation Precipitation comes about when: -warm air rises, cools, loses ability to hold water vapor -water vapor condenses into droplets -water droplets form clouds -heavy clouds release droplets as rain, snow continued Weather Continued...

SECTION 1 NEXT Precipitation Three types of precipitation -convectional -orthographic -frontal Rain shadow—land on leeward side of hills, mountains -little precipitation in rain shadow continued Weather Continued...

SECTION 1 NEXT Hurricanes Huge storms called hurricanes, or typhoons in Asia: -form over warm, tropical ocean waters -hit land with heavy rain, high winds, storm surge Tornadoes Tornado—a powerful, funnel-shaped column of spiraling air: -born from strong thunderstorms -capable of immense damage continued Weather

SECTION 1 NEXT Weather Extremes Blizzards Blizzard—heavy snowstorm with strong winds, reduced visibility Droughts Drought: long period of time with either no or minimal rainfall Floods Water spreads out over normally dry land

NEXT Section 2 Climate 6 slides Today you will do 9 slides total- 6 in section 2 and 3 in section 3.

Factors Affecting Climate Wind Currents Wind, ocean currents help distribute sun’s heat worldwide Convection—upward motion of air that transfers heat in atmosphere Coriolis effect is the bending of winds due to Earth’s rotation Climate NEXT SECTION 2 Continued...

Ocean Currents Resembles rivers flowing in the ocean Warm water flows away from equator toward poles Cold, polar water flows back toward equator

NEXT Zones of Latitude Low, or tropical latitude -hot all year round Middle, or temperate latitude -warm summers and cold winters High, or polar latitude -cold all year round SECTION 2 continued Factors Affecting Climate Continued...

SECTION 2 NEXT Elevation Elevation is the distance above sea level As elevation increases, climate gets colder Topography Topography: landforms and their distribution in an area Landforms, especially mountains, affect climate continued Factors Affecting Climate

SECTION 2 NEXT Changes in Climate El Niño El Niño—winds push warm Pacific Ocean waters toward the Americas La Niña—winds push warm waters toward Australia and Asia Both cause natural, worldwide changes in climate

Global Warming Gradual warming of the earth’s atmosphere Greenhouse effect—the earth warms due to trapped solar energy

NEXT Section 3 World Climate Regions 5 slides

Typical Weather Temperature and precipitation define climate Location, topography, elevation may impact climate Five general climate regions: -tropical (low-latitude) -dry -mid-latitude -high latitude -highland Defining a Climate Region NEXT SECTION 3

Types of Climates Tropical Wet Always hot; daily rainfall adds up to more than 80” annually NEXT SECTION 3 Tropical Wet and Dry Warm, wet summer season; cooler, dry winter season Continued... Semiarid Hot summers; mild to cold winters; little precipitation

Desert Two kinds of desert—hot, cool/cold; less than 10” rain per year Mediterranean Summers dry and hot; winters cool and rainy Marine West Coast Moderate temperatures; frequently cloudy, foggy, damp Humid Subtropical Long periods of summer heat and humidity; winters mild to cool

Humid Continental Great variety of temperature, precipitation; four distinct seasons Subarctic Summers are short and cool; winters are long and very cold Tundra Tundra—flat, treeless ring of lands around the Arctic Ocean Very little precipitation; summer temperatures around 40°F. Permafrost is the constantly frozen subsoil found in this region

SECTION 3 Ice Cap Snow, ice, permanently freezing temperatures continued Types of Climates Highlands Climate varies with latitude, elevation, topography, location

NEXT Section 4 Soils and Vegetation 7 slides

Soil Regions Shaping Human Existence Soil is a thin layer of weathered rock, humus, air, water Topsoil refers to the top 6” of soil Soil characteristics vary with climate Type of soil determines type of vegetation that can be supported Type of vegetation determines type of possible human activity Soils and Vegetation NEXT SECTION 4

Vegetation Regions Natural Environments Ecosystem—interdependent community of plants and animals Biome—the ecosystem of a region Biomes are further divided into: -forest -grassland -desert -tundra NEXT SECTION 4 Continued...

NEXT SECTION 4 Forestlands Forest regions categorized by trees they support—broadleaf or needle Deciduous—broadleaf trees: maple, oak, birch, cottonwood -mostly in Northern Hemisphere Rain forest—tropical forest covered with broadleaf trees continued Vegetation Regions Continued...

Coniferous—needle leaf trees; cone bearing: pine, fir, cedar -mostly in Northern Hemisphere Deciduous and coniferous trees together form mixed forest

NEXT SECTION 4 Grasslands Flat regions with few trees A savanna is a tropical grassland Steppe, or prairie, are temperate grasslands of Northern Hemisphere continued Vegetation Regions

Desert and Tundra Plants in these regions have adapted to climate extremes: -tundra plants (mosses, lichen) hug the ground -desert plants (cacti, sagebrush) conserve water, withstand heat

Human Impact on the Environment NEXT SECTION 4 Altering the Landscape Humans either adapt to land, or alter it to meet their needs Some human activities that affect the environment: -building dams -installing irrigation systems -planting crops -slashing and burning vegetation