Chapter 3 Physical Geography Climate and Vegetation Climate is created by the sun’s solar energy interacting with the earth’s land, water, and air. In.

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Presentation transcript:

Chapter 3 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.

Index Section 1: Seasons and Weather Section 2: Climate Section 3: World Climate Regions Section 4: Soils and Vegetation

Seasons and Weather Seasons and weather occur because of the changing position of the earth in relation to the sun. Weather extremes are related to location on earth.

Seasons 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

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

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

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

Precipitation Three types of precipitation

Hurricanes and Tornadoes 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

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 spread out over normally dry land

Section 2: Climate Climate reflects the seasonal patterns of weather for a location over a long period of time. Global climatic changes may be natural or human-made.

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

Factors Affecting Climate Ocean Currents Resemble rivers flowing in the ocean Warm water flows away from equator toward poles Cold, polar water flows back toward equator

Factors Affecting Climate 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

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

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

Section 3: World Climate Regions Temperature and precipitation define climate regions. Broad climate definitions help to identify variations in weather at a location over the course of a year.

Defining a Climate Region 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

Types of Climates Tropical Wet Always hot; daily rainfall adds up to more than 80” annually Tropical Wet and Dry Warm, wet summer season; cooler, dry winter season Semiarid Hot summers; mild to cold winters; little precipitation Desert Two kinds of desert—hot, cool/cold; less than 10” rain per year

Types of Climates 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

Types of Climates 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 Ice Cap Snow, ice, permanently freezing temperatures

Types of Climates

Highlands Climate varies with latitude, elevation, topography, location

Section 4: Soils and Vegetation Soil and climate help to determine the vegetation of a region. Human land use alters the vegetation in both positive and negative ways.

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

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

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

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

Vegetation Regions

Human Impact on the Environment 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