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8.1: Climate and Biomes

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    32173
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    Biomes are large-scale environments that are distinguished by characteristic climate and vegetation (figure \(\PageIndex{a}\)). Biomes are also characterized by the animals and other organisms there, which are influenced by vegetation and climate patterns. The Earth’s biomes are categorized into two major groups: terrestrial and aquatic. Terrestrial biomes are based on land, while aquatic biomes include both ocean and freshwater biomes. Altitude and latitude, which affect temperature and precipitation determine the distribution of biomes. 

    Graph showing how annual temperature and precipitation determine biomes
    Figure \(\PageIndex{a}\): Average annual temperature and annual precipitation are two climatic factors that determine the distribution of biomes. This graph shows annual precipitation in centimeters on the y-axis and average annual temperature in degrees Celsius on the x-axis. Tropical rainforests have the highest temperatures and most precipitation. Tropical seasonal forests and savannas have high temperatures (20-30°C) with precipitation from approximately 50 to 270 centimeters. Subtropical deserts have similarly high temperatures but dry conditions. Temperate grasslands and cold deserts range in average annual temperature from below 0 to 22°C and have less than 50 centimeters of precipitation per year. Woodlands/shrublands (such as the chaparral) have the same temperature range as cold deserts but can receive a little over 100 cm of precipitation per year. Temperate forests have intermediate temperatures (approximately 16-22°C), but temperate rainforests receive more precipitation than temperate seasonal forests. Boreal forests receive a little less precipitation than temperate forests, but are colder (approximately 1-10°C). The tundra has the coldest temperatures and little precipitation. Deserts have a range of temperatures but low precipitation. Image by Navarras (public domain).

    Low latitudes (near the equator) have high temperatures, while high latitudes (near the poles) have low temperatures. This is because the sun hits the equator more directly. Sunlight hits the poles at an angle, reducing the intensity of light (and heat energy) per unit of area. Temperature also decreases with altitude. At high altitudes, the atmosphere is thinner and traps less heat energy from the sun. Because temperatures decline with altitude as well as latitude, similar biomes exist on mountains even when they are at low latitudes. As a rule of thumb, a climb of 1000 feet (about 300 m) is equivalent in changed flora and fauna to a trip northward of some 600 miles (966 km). 

    Where precipitation is moderately abundant — 40 inches (about 1 m) or more per year — and distributed fairly evenly throughout the year, the major determinant is temperature. It is not simply a matter of average temperature, but includes such limiting factors as whether it ever freezes or length of the growing season. Biomes are thus characterized not only by average temperature and precipitation but also their seasonality.

    Not only does latitude influence temperature, but it also affects precipitation. For example, deserts tend to occur at latitudes of around 30° and at the poles, both north and south, driven by circulation and prevailing wind patterns in the atmosphere. The engine that drives circulation in the atmosphere and oceans is solar energy, which is determined by the average position of the sun over the Earth’s surface. Direct light provides uneven heating depending on latitude and angle of incidence, with high solar energy in the tropics, and little or no energy at the poles. Atmospheric circulation and geographic location are the primary causal agents of deserts. At approximately 30° north and south of the equator, sinking air produces trade wind deserts like the Sahara and the Outback of Australia (figure \(\PageIndex{b}\)). 

    Air circulation patterns diagrammed on the Earth
    Figure \(\PageIndex{b}\): The generalized circulation of the atmosphere. Solar energy falling on the equatorial belt heats the air and causes it to rise. The rising air cools and its contained moisture falls back on the tropics as rain. The drier air then continues to spread toward the north and south where it sinks back at about 30 degrees north and south latitudes. This sinking drier air creates belts of predominant high pressure along which desert conditions prevail. These belts of predominantly high pressure have air that descends along these belts and flows either north to become the westerlies or south to become the trade winds. Note the arrows indicating general directions of winds in the latitude zones. The trade winds are predominant in the tropics and the westerlies in the mid-latitudes.

    The MinuteEarth video below discusses the global climate patterns which lead to deserts.

    Rainshadow deserts are produced where prevailing winds with moist air dries as it is forced to rise over mountains. The prevailing winds in the western half of North America blow in from the Pacific laden with moisture. Each time this air rises up from the western slopes of, successively, the Coast Ranges, the Sierras and Cascades, and finally the Rockies, it cools and its capacity to hold moisture decreases. The excess moisture condenses to rain or snow, which drenches the mountain slopes beneath. When the air reaches the eastern slopes, it is relatively dry, and much less precipitation falls. This phenomenon is called the rainshadow effect (figure \(\PageIndex{c}\)). How much rain falls and when influences the type of biome. For example, the Great Basin Desert (figure \(\PageIndex{d}\)) is a rain shadow desert produced as moist air from the Pacific rises by lifting over the Sierra Nevada Mountain (and other) and loses moisture from previous condensation and precipitation on the rainy side of the range(s). 

    Prevaling winds bring moist air over a mountain, where it cools and precipitates. Dry air on the side of the mountain causes a desert.
    Figure \(\PageIndex{c}\): The rain shadow effect. Warm, moist air is carried up a mountain by prevailing winds. The rising air cools and condenses, resulting in precipitation as it moves up the mountain. The dry air advances down the other side of the mountain, resulting in a rain shadow (a dry region). Image by domdomegg (CC-BY).
    Map of the area covers most of Nevada, easternmost California, southern Idaho, and western Utah
    Figure \(\PageIndex{d}\): Map of the Great Basin Desert. Image by USGS (public domain).

    Attributions

    Modified by Melissa Ha from the following sources:


    This page titled 8.1: Climate and Biomes is shared under a CC BY-NC-SA 4.0 license and was authored, remixed, and/or curated by Melissa Ha and Rachel Schleiger (ASCCC Open Educational Resources Initiative) .

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