Soil Carbon Feedback - Revision history

Florez4747: /* Related */

2023-06-21T18:51:02Z

← Older revision		Revision as of 18:51, 21 June 2023
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	= Related =		= Related =
	[[Carbon Stocks]]		[[Carbon Stocks]]; [[Carbon cycle]]

	= Uncertainties =		= Uncertainties =

Florez4747 at 17:27, 21 June 2023

2023-06-21T17:27:50Z

← Older revision		Revision as of 17:27, 21 June 2023
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	"The soil carbon feedback concerns the releases of carbon from soils in response to global warming. This response under climate change is a positive climate feedback. There is approximately two to three times more carbon in global soils than the Earth's atmosphere,[1][2] which makes understanding this feedback crucial to understand future climate change. An increased rate of soil respiration is the main cause of this feedback, where measurements imply that 4 °C of warming increases annual soil respiration by up to 37%.[3]"<Ref>https://en.wikipedia.org/wiki/Soil_carbon_feedback</Ref>		"The soil carbon feedback concerns the releases of carbon from soils in response to global warming. This response under climate change is a positive climate feedback. There is approximately two to three times more carbon in global soils than the Earth's atmosphere,[1][2] which makes understanding this feedback crucial to understand future climate change. An increased rate of soil respiration is the main cause of this feedback, where measurements imply that 4 °C of warming increases annual soil respiration by up to 37%.[3]"<Ref>https://en.wikipedia.org/wiki/Soil_carbon_feedback</Ref>


			= Related =
			[[Carbon Stocks]]

	= Uncertainties =		= Uncertainties =

Florez4747 at 01:17, 17 March 2023

2023-03-17T01:17:22Z

← Older revision		Revision as of 01:17, 17 March 2023
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	= Uncertainties =		= Uncertainties =
	Many climate models to not account for feedback loops relating to carbon released from soil triggered by increased temperatures.<Ref>S. Wieczorek, P. Ashwin, C. M. Luke, P. M. Cox (2011). "Excitability in ramped systems: the compost-bomb instability". Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences. The Royal Society. 467 (2129): 1243–1269. Bibcode:2011RSPSA.467.1243W. doi:10.1098/rspa.2010.0485</Ref> A limitation in our understanding of carbon cycling comes from the insufficient incorporation of soil animals, including insects and worms, and their interactions with microbial communities into global decomposition models.<Ref>Crowther, Thomas W.; Thomas, Stephen M.; Maynard, Daniel S.; Baldrian, Petr; Covey, Kristofer; Frey, Serita D.; Diepen, Linda T. A. van; Bradford, Mark A. (2015-05-14). "Biotic interactions mediate soil microbial feedbacks to climate change". Proceedings of the National Academy of Sciences. 112 (22): 7033–7038. Bibcode:2015PNAS..112.7033C. doi:10.1073/pnas.1502956112. ISSN 0027-8424. PMC 4460469. PMID 26038557</Ref><Ref>Lewis, Renee (2015-05-19). "The diet of worms: Soil dwellers emerge as climate change heroes in study". america.aljazeera.com. Retrieved 2021-11-30</Ref>		Many climate models to not account for feedback loops relating to carbon released from soil triggered by increased temperatures.<Ref>S. Wieczorek, P. Ashwin, C. M. Luke, P. M. Cox (2011). "Excitability in ramped systems: the compost-bomb instability". Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences. The Royal Society. 467 (2129): 1243–1269. Bibcode:2011RSPSA.467.1243W. doi:10.1098/rspa.2010.0485</Ref> A limitation in our understanding of carbon cycling comes from the insufficient incorporation of soil animals, including insects and worms, and their interactions with microbial communities into global decomposition models.<Ref>Crowther, Thomas W.; Thomas, Stephen M.; Maynard, Daniel S.; Baldrian, Petr; Covey, Kristofer; Frey, Serita D.; Diepen, Linda T. A. van; Bradford, Mark A. (2015-05-14). "Biotic interactions mediate soil microbial feedbacks to climate change". Proceedings of the National Academy of Sciences. 112 (22): 7033–7038. Bibcode:2015PNAS..112.7033C. doi:10.1073/pnas.1502956112. ISSN 0027-8424. PMC 4460469. PMID 26038557</Ref><Ref>Lewis, Renee (2015-05-19). "The diet of worms: Soil dwellers emerge as climate change heroes in study". america.aljazeera.com. Retrieved 2021-11-30</Ref>

			= Tipping Points =

			== Peatlands ==

	= Sources =		= Sources =

Florez4747: /* Uncertainties */

2023-03-16T17:10:22Z

Uncertainties

← Older revision		Revision as of 17:10, 16 March 2023
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	= Uncertainties =		= Uncertainties =
	Many climate models to not account for feedback loops relating to carbon ~~being~~ released ~~form~~ soil ~~due to~~ increased temperatures.<Ref>S. Wieczorek, P. Ashwin, C. M. Luke, P. M. Cox (2011). "Excitability in ramped systems: the compost-bomb instability". Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences. The Royal Society. 467 (2129): 1243–1269. Bibcode:2011RSPSA.467.1243W. doi:10.1098/rspa.2010.0485</Ref> A limitation in our understanding of carbon cycling comes from the insufficient incorporation of soil animals, including insects and worms, and their interactions with microbial communities into global decomposition models.<Ref>Crowther, Thomas W.; Thomas, Stephen M.; Maynard, Daniel S.; Baldrian, Petr; Covey, Kristofer; Frey, Serita D.; Diepen, Linda T. A. van; Bradford, Mark A. (2015-05-14). "Biotic interactions mediate soil microbial feedbacks to climate change". Proceedings of the National Academy of Sciences. 112 (22): 7033–7038. Bibcode:2015PNAS..112.7033C. doi:10.1073/pnas.1502956112. ISSN 0027-8424. PMC 4460469. PMID 26038557</Ref><Ref>Lewis, Renee (2015-05-19). "The diet of worms: Soil dwellers emerge as climate change heroes in study". america.aljazeera.com. Retrieved 2021-11-30</Ref>		Many climate models to not account for feedback loops relating to carbon released from soil triggered by increased temperatures.<Ref>S. Wieczorek, P. Ashwin, C. M. Luke, P. M. Cox (2011). "Excitability in ramped systems: the compost-bomb instability". Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences. The Royal Society. 467 (2129): 1243–1269. Bibcode:2011RSPSA.467.1243W. doi:10.1098/rspa.2010.0485</Ref> A limitation in our understanding of carbon cycling comes from the insufficient incorporation of soil animals, including insects and worms, and their interactions with microbial communities into global decomposition models.<Ref>Crowther, Thomas W.; Thomas, Stephen M.; Maynard, Daniel S.; Baldrian, Petr; Covey, Kristofer; Frey, Serita D.; Diepen, Linda T. A. van; Bradford, Mark A. (2015-05-14). "Biotic interactions mediate soil microbial feedbacks to climate change". Proceedings of the National Academy of Sciences. 112 (22): 7033–7038. Bibcode:2015PNAS..112.7033C. doi:10.1073/pnas.1502956112. ISSN 0027-8424. PMC 4460469. PMID 26038557</Ref><Ref>Lewis, Renee (2015-05-19). "The diet of worms: Soil dwellers emerge as climate change heroes in study". america.aljazeera.com. Retrieved 2021-11-30</Ref>

	= Sources =		= Sources =

Florez4747: /* Uncertainties */

2023-03-16T17:09:55Z

Uncertainties

← Older revision		Revision as of 17:09, 16 March 2023
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	= Uncertainties =		= Uncertainties =
	Many climate models to not account for feedback loops relating to carbon being released form soil due to increased temperatures.<Ref>S. Wieczorek, P. Ashwin, C. M. Luke, P. M. Cox (2011). "Excitability in ramped systems: the compost-bomb instability". Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences. The Royal Society. 467 (2129): 1243–1269. Bibcode:2011RSPSA.467.1243W. doi:10.1098/rspa.2010.0485</Ref>		Many climate models to not account for feedback loops relating to carbon being released form soil due to increased temperatures.<Ref>S. Wieczorek, P. Ashwin, C. M. Luke, P. M. Cox (2011). "Excitability in ramped systems: the compost-bomb instability". Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences. The Royal Society. 467 (2129): 1243–1269. Bibcode:2011RSPSA.467.1243W. doi:10.1098/rspa.2010.0485</Ref> A limitation in our understanding of carbon cycling comes from the insufficient incorporation of soil animals, including insects and worms, and their interactions with microbial communities into global decomposition models.<Ref>Crowther, Thomas W.; Thomas, Stephen M.; Maynard, Daniel S.; Baldrian, Petr; Covey, Kristofer; Frey, Serita D.; Diepen, Linda T. A. van; Bradford, Mark A. (2015-05-14). "Biotic interactions mediate soil microbial feedbacks to climate change". Proceedings of the National Academy of Sciences. 112 (22): 7033–7038. Bibcode:2015PNAS..112.7033C. doi:10.1073/pnas.1502956112. ISSN 0027-8424. PMC 4460469. PMID 26038557</Ref><Ref>Lewis, Renee (2015-05-19). "The diet of worms: Soil dwellers emerge as climate change heroes in study". america.aljazeera.com. Retrieved 2021-11-30</Ref>

	= Sources =		= Sources =

Florez4747: Created page with ""The soil carbon feedback concerns the releases of carbon from soils in response to global warming. This response under climate change is a positive climate feedback. There is approximately two to three times more carbon in global soils than the Earth's atmosphere,[1][2] which makes understanding this feedback crucial to understand future climate change. An increased rate of soil respiration is the main cause of this feedback, where measurements imply that 4 °C of warmi..."

2023-03-16T17:08:45Z

Created page with ""The soil carbon feedback concerns the releases of carbon from soils in response to global warming. This response under climate change is a positive climate feedback. There is approximately two to three times more carbon in global soils than the Earth's atmosphere,[1][2] which makes understanding this feedback crucial to understand future climate change. An increased rate of soil respiration is the main cause of this feedback, where measurements imply that 4 °C of warmi..."

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"The soil carbon feedback concerns the releases of carbon from soils in response to global warming. This response under climate change is a positive climate feedback. There is approximately two to three times more carbon in global soils than the Earth's atmosphere,[1][2] which makes understanding this feedback crucial to understand future climate change. An increased rate of soil respiration is the main cause of this feedback, where measurements imply that 4 °C of warming increases annual soil respiration by up to 37%.[3]"<Ref>https://en.wikipedia.org/wiki/Soil_carbon_feedback</Ref>

= Uncertainties =
Many climate models to not account for feedback loops relating to carbon being released form soil due to increased temperatures.<Ref>S. Wieczorek, P. Ashwin, C. M. Luke, P. M. Cox (2011). "Excitability in ramped systems: the compost-bomb instability". Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences. The Royal Society. 467 (2129): 1243–1269. Bibcode:2011RSPSA.467.1243W. doi:10.1098/rspa.2010.0485</Ref>

= Sources =