microclimates
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The Sahara Desert is a non-example of a microclimate because it is a large and distinct region with extreme weather conditions that affect a wide area, rather than a small and localized microclimate.
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A microclimate can affect crop production by influencing factors such as temperature, rainfall, humidity, and sunlight exposure. For example, a microclimate that experiences higher temperatures and less rainfall than the surrounding area may lead to increased water stress in crops. On the other hand, a microclimate with ideal conditions can support better growth and yield of crops.
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A microclimate is a small area with a different climate to the other areas around it. Microclimates can vary in size but usually stay quite small.
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No, the desert climate is a major climate zone and not an example of a microclimate. There are, however, microclimates found in deserts.
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A microclimate has features such as proximity to water, a south-sloping location, protection from winds, much bare rock and/or other features that typically increase or moderate the temperature in that location.
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Microclimate is basically defined as the local climate present in a small site or habitat. The microclimate of a place is usually uniform through the year. The term microclimate is usually used to refer to the climate of a place such as a house, a city, a cave or a valley, that is different from the climate in the general larger area. The localised climatic conditions within an urban area or a neighbourhood, differ significantly from the general climatic conditions prevalent in the general urban area or neighbourhood. Stands of trees or shrubs often cause microclimates. Microclimate also refers to the area that directly surrounds the defined area. It can affect the character of the wineproduced in the area which is in the vicinity of the area defined under the scope of the particular microclimate. It also takes into consideration such factors as the warmth and humidity in the air.
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such small-scale differences in climate result in a microclimed.
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Location can affect a microclimate. Anything from the gradient of the landscape to the immediate environment can affect a microclimate. Those located in urban centers may experience more heat as a result of concrete and asphalt which absorb sunlight and heat up the area. Conversely, microclimates located near large bodies of water will benefit from the cooling effect.
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Mountain valleys can produce a microclimate due to their unique topography which can result in temperature inversions. This occurs when cooler air becomes trapped at lower elevations, causing temperature variations within the valley. Additionally, mountainous terrain can influence wind patterns, precipitation, and sunlight exposure, further shaping the microclimate of the valley.
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Microclimates can impact people by affecting their comfort, health, and safety. For example, a hot and humid microclimate can make individuals more susceptible to heat-related illnesses. Conversely, a cold and windy microclimate can increase the risk of hypothermia. Additionally, changes in microclimates due to urban development or deforestation can also impact local ecosystems and biodiversity.
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Water can moderate temperature changes in a microclimate because it has a high specific heat capacity, meaning it can absorb and release heat slowly. Bodies of water, such as lakes or oceans, can create local differences in temperature by cooling the air in hot weather and warming it in cold weather. Evaporation from water sources can also increase humidity levels and influence precipitation patterns in a microclimate.
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The term for a climate in a specific region that varies from the climate of the surrounding region is known as a microclimate. Microclimates can be influenced by factors such as topography, proximity to bodies of water, and human activity.
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YES
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An example of a microclimate is a small area within a city that is significantly warmer than surrounding areas due to the presence of concrete and buildings, which absorb and retain heat. This can create a "heat island" effect, leading to higher temperatures in that specific location compared to its surroundings.
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relative humidity, air temperature, solar radiance and wind direction
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cooler and receive less direct sunlight than north-facing slopes. This can lead to differences in temperature, humidity, and vegetation between the two slopes, creating a unique microclimate.
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A microclimate can create a microhabitat by influencing factors such as temperature, humidity, and light levels in a small area. These unique conditions can lead to the presence of specific plant and animal species that are adapted to thrive in that particular microclimate. For example, a sunny, sheltered corner of a garden may provide a warmer and less windy environment, creating a microhabitat suitable for delicate plant species or insects.
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South-facing mountains in the Northern Hemisphere receive more direct sunlight, leading to warmer temperatures compared to the north-facing slopes. This exposure to sunlight creates a microclimate that is typically drier and sunnier, allowing for different vegetation to thrive and supporting unique ecosystems.
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South facing mountain slopes in the northern hemisphere receive more sunlight compared to north facing slopes, leading to higher temperatures and drier conditions. This creates a microclimate that can support different vegetation and wildlife compared to the cooler and more shaded north facing slopes.
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South-facing mountain slopes receive more direct sunlight and warmth, creating a drier and warmer microclimate compared to north-facing slopes. This results in faster snowmelt and higher temperatures, which can support different plant and animal species adapted to these conditions.
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an example would be..............
sea breezes often make beaches cooler than a nearby inland areas on a warm afternoon!!
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No, they can live in temperate climates too. Also where humans create a microclimate (in their homes), cockroaches can also live.
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Microclimates are small-scale areas within a larger region that have different climate conditions, typically due to variations in factors like elevation, proximity to bodies of water, and landscape features. These variations can lead to differences in temperature, humidity, and precipitation within a relatively small area, resulting in the formation of distinct microclimates.
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Microclimates can be produced by the presence of landforms such as rivers and lakes. They can also be influenced by local activity of human beings. Farming can change the microclimate of an area.
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Adil Al-Kindy has written:
'Macro and microclimate effects on cover zone properties of field cured concrete'
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A micro climate is the average temperature in a small area and a climate is the average temperature in a large area. And near bodies of water which may cool the local atmosphere, or in heavy urban areas where brick, concrete, and asphalt absorb the sun's energy, heat up, and re-radiate that heat to the ambient air: the resulting urban heat island is a kind of microclimate.
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A valley can produce a microclimate by trapping cooler air near the valley floor due to its topographic features, resulting in temperature inversions. In addition, valleys may shield the area from strong winds, leading to calmer conditions and potentially higher humidity levels. The shape and orientation of the valley can also affect the amount of sunlight and precipitation received, influencing the local climate.
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Ph Stoutjesdijk has written:
'Microclimate, vegetation and fauna' -- subject(s): Microclimatology, Biotic communities, Vegetation and climate, Plant-atmosphere relationships
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Human factors can affect microclimates by altering land use patterns, such as urbanization leading to the urban heat island effect. Human activities like transportation and industry can also release pollutants that affect air quality and temperature, impacting local microclimates. Additionally, changes in vegetation, such as deforestation or agriculture, can influence temperature, humidity, and wind patterns in a microclimate.
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dry and warmer
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a city with tall buildings creating urban heat islands, leading to higher temperatures compared to surrounding areas.
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A large lake is generally warm and has a lot of moisture, we find that it generates this very big convective potential energy, which generates a lot of cloudness and this unique nature of weather characterized by heavy thunderstorms.
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David Leslie Spittlehouse has written:
'Using data loggers in the field' -- subject(s): Forests and forestry, Measurement
'Seedling microclimate' -- subject(s): Forest microclimatology
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A microclimate can impact crop production by affecting temperature, humidity, wind, and precipitation differently within a small area. For example, a valley may experience cooler temperatures than surrounding areas, affecting the growth of certain crops sensitive to colder conditions. Additionally, microclimates can create variations in sunlight exposure, which may impact crop growth and development.
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Modern meteorology has provided more comprehensive data on the climate in specific locations. Farmers now have specific climatic information on their particular microclimate, rather than having to rely on regional data and averages.
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California is a big state with large variations in microclimate. You'll need to be more specific as to where in California you're talking about.
It's a good bet that California will be less humid. Other than that it's hard to say.
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You can see snow on the top of Mt. Kilimanjaro, which is a mountain near the border of Kenya and Tanzania -- near the equator on the east side of Africa. The snow is due to the high altitude and the microclimate created by the mountain range which includes Kilimanjaro, Kenya and Meru.
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Topography would relate more to microclimate: 'the physical state of the atmosphere close to a very small area of the earth's surface.." The sunny side of hills will be warmer, the shady side cooler, etc. http://www.bbc.co.uk/weather/features/understanding/microclimates.shtml
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Penguins huddle together to keep warm because they can share body heat and reduce heat loss to the environment. By forming a tight group, they create a microclimate that helps them survive in cold conditions.
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this is a local atmospheric zone where the climate differs from the surrounding area. It may be a few square feet or an area very much larger. For example an area may be affected by a body of water which may cool the temperature near to the water, but may be much higher some distance away
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