Microclimate - Revision history

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2023-05-10T18:07:01Z

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← Older revision		Revision as of 14:07, 10 May 2023
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	The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) elevation, successional stage, vegetation and canopy presence[4,5]. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]		The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) elevation, successional stage, vegetation and canopy presence[4,5]. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]
	==In Soils==		==In Soils==
	Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. Microclimate, especially temperature and moisture, regulates activity rates of decomposers[7]. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [6] This high heterogeneity of conditions may contribute to high overall [[biodiversity interactions\|soil biodiversity]] as well.		Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. Microclimate, especially temperature and moisture, regulates activity rates of [[decomposers]][7]. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [6] This high heterogeneity of conditions may contribute to high overall [[biodiversity interactions\|soil biodiversity]] as well.

	Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[3] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events. Soil texture greatly influences local microclimate by regulating availability of surface water films and water-holding capacity [7].		Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[3] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events. Soil texture greatly influences local microclimate by regulating availability of surface water films and water-holding capacity [7].

Njhenshu: The LinkTitles extension automatically added links to existing pages (https://github.com/bovender/LinkTitles).

2023-03-31T18:29:04Z

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	5. Frey, S. J. K., Hadley, A. S. & Betts, M. G. Microclimate predicts within-season distribution dynamics of montane forest birds. ''[[Diversity]] Distrib''. '''22''', 944–959 (2016).		5. Frey, S. J. K., Hadley, A. S. & Betts, M. G. Microclimate predicts within-season distribution dynamics of montane forest birds. ''[[Diversity]] Distrib''. '''22''', 944–959 (2016).

	6. Kraichak, E. Microclimate Fluctuation Correlated with Beta Diversity of Epiphyllous Bryophyte Communities. ''Biotropica'' '''46''', 575–582 (2014).		6. Kraichak, E. Microclimate Fluctuation Correlated with Beta Diversity of Epiphyllous [[Bryophyte]] Communities. ''Biotropica'' '''46''', 575–582 (2014).

	7. Coleman, David C., Callaham Jr., Mac A., and Crossley Jr., D. A. “Fundamentals of [[Soil Ecology]], Third Edition.” 2018. Academic Press. Cambridge, MA.		7. Coleman, David C., Callaham Jr., Mac A., and Crossley Jr., D. A. “Fundamentals of [[Soil Ecology]], Third Edition.” 2018. Academic Press. Cambridge, MA.

Ajacobs5: /* References */

2021-05-14T20:27:25Z

References

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	6. Kraichak, E. Microclimate Fluctuation Correlated with Beta Diversity of Epiphyllous Bryophyte Communities. ''Biotropica'' '''46''', 575–582 (2014).		6. Kraichak, E. Microclimate Fluctuation Correlated with Beta Diversity of Epiphyllous Bryophyte Communities. ''Biotropica'' '''46''', 575–582 (2014).

			7. Coleman, David C., Callaham Jr., Mac A., and Crossley Jr., D. A. “Fundamentals of [[Soil Ecology]], Third Edition.” 2018. Academic Press. Cambridge, MA.

Ajacobs5: /* In Soils */

2021-05-14T20:26:33Z

In Soils

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	The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) elevation, successional stage, vegetation and canopy presence[4,5]. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]		The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) elevation, successional stage, vegetation and canopy presence[4,5]. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]
	==In Soils==		==In Soils==
	Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. Microclimate, especially temperature and moisture, regulates activity rates of decomposers[9]. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [6] This high heterogeneity of conditions may contribute to high overall [[biodiversity interactions\|soil biodiversity]] as well.		Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. Microclimate, especially temperature and moisture, regulates activity rates of decomposers[7]. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [6] This high heterogeneity of conditions may contribute to high overall [[biodiversity interactions\|soil biodiversity]] as well.

	Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[3] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events. Soil texture greatly influences local microclimate by regulating availability of surface water films and water-holding capacity [9].		Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[3] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events. Soil texture greatly influences local microclimate by regulating availability of surface water films and water-holding capacity [7].

	==References==		==References==

Ajacobs5: /* In Soils */

2021-05-14T20:26:17Z

In Soils

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	The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) elevation, successional stage, vegetation and canopy presence[4,5]. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]		The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) elevation, successional stage, vegetation and canopy presence[4,5]. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]
	==In Soils==		==In Soils==
	Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [6] This high heterogeneity of conditions may contribute to high overall [[biodiversity interactions\|soil biodiversity]] as well.		Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. Microclimate, especially temperature and moisture, regulates activity rates of decomposers[9]. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [6] This high heterogeneity of conditions may contribute to high overall [[biodiversity interactions\|soil biodiversity]] as well.
	Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[3] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events.
			Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[3] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events. Soil texture greatly influences local microclimate by regulating availability of surface water films and water-holding capacity [9].

	==References==		==References==

Ajacobs5 at 19:21, 7 May 2021

2021-05-07T19:21:12Z

Ajacobs5: /* In Soils */

2021-05-05T19:48:48Z

In Soils

← Older revision		Revision as of 15:48, 5 May 2021
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	The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) successional stage, vegetation and canopy presence. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]		The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) successional stage, vegetation and canopy presence. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]
	==In Soils==		==In Soils==
	Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [8] This high heterogeneity of conditions may contribute to high overall soil biodiversity as well.		Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [8] This high heterogeneity of conditions may contribute to high overall [[biodiversity interactions\|soil biodiversity]] as well.
	Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[4] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events.		Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[4] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events.

Ajacobs5: /* In Soils */

2021-05-05T19:47:41Z

In Soils

← Older revision		Revision as of 15:47, 5 May 2021
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	The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) successional stage, vegetation and canopy presence. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]		The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) successional stage, vegetation and canopy presence. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]
	==In Soils==		==In Soils==
	Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. High fluctuations in microclimate has been shown to lead to high bryophyte diversity. [8] This high heterogeneity of conditions may contribute to high overall soil biodiversity as well.		Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [8] This high heterogeneity of conditions may contribute to high overall soil biodiversity as well.
	Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[4] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events.		Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[4] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events.

Ajacobs5: /* References */

2021-05-05T19:41:40Z

References

← Older revision		Revision as of 15:41, 5 May 2021
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	4. Cécillon, L., de Mello, N. A., De Danieli, S. & Brun, J.-J. Soil macroaggregate dynamics in a mountain spatial climate gradient. ''Biogeochemistry'' '''97''', 31–43 (2010).		4. Cécillon, L., de Mello, N. A., De Danieli, S. & Brun, J.-J. Soil macroaggregate dynamics in a mountain spatial climate gradient. ''Biogeochemistry'' '''97''', 31–43 (2010).

	~~5. Kaufman, D. W., Peterson, S. K., Fristik, R. & Kaufman, G. A. Effect of Microhabitat Features on Habitat Use by Peromyscus leucopus. ''American Midland Naturalist'' '''110''', 177 (1983).~~

	6. Tsuyuzaki, S., Matsuda, M. & Akasaka, M. Effect of a deciduous shrub on microclimate along an elevation gradient, Mount Koma, northern Japan. ''Clim. Res''. '''51''', 1–10 (2012).		6. Tsuyuzaki, S., Matsuda, M. & Akasaka, M. Effect of a deciduous shrub on microclimate along an elevation gradient, Mount Koma, northern Japan. ''Clim. Res''. '''51''', 1–10 (2012).

Ajacobs5: /* References */

2021-05-05T19:38:54Z

References

← Older revision		Revision as of 15:38, 5 May 2021
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	2. Breshears, D. D., Nyhan, J. W., Heil, C. E. & Wilcox, B. P. Effects of Woody Plants on Microclimate in a Semiarid Woodland: Soil Temperature and Evaporation in Canopy and Intercanopy Patches. ''International Journal of Plant Sciences'' '''159''', 1010–1017 (1998).		2. Breshears, D. D., Nyhan, J. W., Heil, C. E. & Wilcox, B. P. Effects of Woody Plants on Microclimate in a Semiarid Woodland: Soil Temperature and Evaporation in Canopy and Intercanopy Patches. ''International Journal of Plant Sciences'' '''159''', 1010–1017 (1998).

	3. Blackith, R. M. Interrelationships between Small [[Arthropods]] and [[Nematodes]] in Peat. ''Proceedings of the Royal Irish Academy, Section B: Biological, Geological, and Chemical Science'' '''75''', 12 (1975).

	4. Cécillon, L., de Mello, N. A., De Danieli, S. & Brun, J.-J. Soil macroaggregate dynamics in a mountain spatial climate gradient. ''Biogeochemistry'' '''97''', 31–43 (2010).		4. Cécillon, L., de Mello, N. A., De Danieli, S. & Brun, J.-J. Soil macroaggregate dynamics in a mountain spatial climate gradient. ''Biogeochemistry'' '''97''', 31–43 (2010).

← Older revision		Revision as of 15:21, 7 May 2021
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	Microclimate is the set of atmospheric conditions that occur in a local area as a result of environmental heterogeneity near the Earth’s surface. Microclimates play an integral role in ecosystem processes. Microclimatic variations in energy and moisture directly affect a number of key ecological processes in forest ecosystems occurring at multiple spatial and temporal scales. [[File:Microclimate1.png\|400px\|thumb\|right\|Schematic of microclimatic processes relating to heat and water transfer of an organism, [1] ]]		Microclimate is the set of atmospheric conditions that occur in a local area as a result of environmental heterogeneity near the Earth’s surface. Microclimates play an integral role in ecosystem processes. Microclimatic variations in energy and moisture directly affect a number of key ecological processes in forest ecosystems occurring at multiple spatial and temporal scales. [[File:Microclimate1.png\|400px\|thumb\|right\|Schematic of microclimatic processes relating to heat and water transfer of an organism, [1] ]]
	==Influences on Microclimate==		==Influences on Microclimate==
	The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) successional stage, vegetation and canopy presence. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]		The two major sources of microclimate variability are differences in energy and moisture, or temperature and humidity. Differences in temperature and humidity can have numerous drivers, including aspect, (direction that a slope faces,) elevation, successional stage, vegetation and canopy presence[4,5]. The presence of bodies of water can influence microclimate, as they may increase humidity and stabilize temperature. Presence of herbaceous and woody vegetation can also greatly influence microclimate, as they create structure and shade. [2]
	==In Soils==		==In Soils==
	Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [8] This high heterogeneity of conditions may contribute to high overall [[biodiversity interactions\|soil biodiversity]] as well.		Consideration of the microclimate is particularly important in [[soil]] [[ecology]], as the heterogenous nature of soil means that numerous microclimates are present in very small areas of soils. High fluctuations in microclimate has been shown to lead to high [[moss\|bryophyte]] diversity. [6] This high heterogeneity of conditions may contribute to high overall [[biodiversity interactions\|soil biodiversity]] as well.
	Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[4] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events.		Soil microclimate can affect macroaggregate dynamics and [[Aggregate formation]].[3] Soil erodability is reduced in warmer climates, which prevents the occurrence of fragile microaggregates caused by freeze-thaw events.

	==References==		==References==
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	2. Breshears, D. D., Nyhan, J. W., Heil, C. E. & Wilcox, B. P. Effects of Woody Plants on Microclimate in a Semiarid Woodland: Soil Temperature and Evaporation in Canopy and Intercanopy Patches. ''International Journal of Plant Sciences'' '''159''', 1010–1017 (1998).		2. Breshears, D. D., Nyhan, J. W., Heil, C. E. & Wilcox, B. P. Effects of Woody Plants on Microclimate in a Semiarid Woodland: Soil Temperature and Evaporation in Canopy and Intercanopy Patches. ''International Journal of Plant Sciences'' '''159''', 1010–1017 (1998).

	4. Cécillon, L., de Mello, N. A., De Danieli, S. & Brun, J.-J. Soil macroaggregate dynamics in a mountain spatial climate gradient. ''Biogeochemistry'' '''97''', 31–43 (2010).		3. Cécillon, L., de Mello, N. A., De Danieli, S. & Brun, J.-J. Soil macroaggregate dynamics in a mountain spatial climate gradient. ''Biogeochemistry'' '''97''', 31–43 (2010).

	6. Tsuyuzaki, S., Matsuda, M. & Akasaka, M. Effect of a deciduous shrub on microclimate along an elevation gradient, Mount Koma, northern Japan. ''Clim. Res''. '''51''', 1–10 (2012).		4. Tsuyuzaki, S., Matsuda, M. & Akasaka, M. Effect of a deciduous shrub on microclimate along an elevation gradient, Mount Koma, northern Japan. ''Clim. Res''. '''51''', 1–10 (2012).

	7. Frey, S. J. K., Hadley, A. S. & Betts, M. G. Microclimate predicts within-season distribution dynamics of montane forest birds. ''[[Diversity]] Distrib''. '''22''', 944–959 (2016).		5. Frey, S. J. K., Hadley, A. S. & Betts, M. G. Microclimate predicts within-season distribution dynamics of montane forest birds. ''[[Diversity]] Distrib''. '''22''', 944–959 (2016).

	8. Kraichak, E. Microclimate Fluctuation Correlated with Beta Diversity of Epiphyllous Bryophyte Communities. ''Biotropica'' '''46''', 575–582 (2014).		6. Kraichak, E. Microclimate Fluctuation Correlated with Beta Diversity of Epiphyllous Bryophyte Communities. ''Biotropica'' '''46''', 575–582 (2014).