Marine Impacts of Climate Change - Revision history

Youarethecause at 14:02, 11 July 2018

2018-07-11T14:02:59Z

← Older revision		Revision as of 14:02, 11 July 2018
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	“Rising atmospheric carbon dioxide (CO2) is one of the most critical problems because its effects are globally pervasive and irreversible on ecological timescales. The primary direct consequences are increasing ocean temperatures <ref> Bindoff, N.L., J. Willebrand, V. Artale, A, Cazenave, J. Gregory, S. Gulev, K. Hanawa, C. Le Quéré, S. Levitus, Y. Nojiri, C.K. Shum, L.D. Talley and A. Unnikrishnan, 2007: Observations: Oceanic Climate Change and Sea Level. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA </ref> and acidity. <ref>[https://imedea.uib-csic.es/master/cambioglobal/Modulo_III_cod101608/Tema_8-acidificación/pH/annurev.marine.010908.163834.pdf] Doney,S. C., Fabry, V. J., Feely, R. A. and Kleypas J. A. (2009) Ocean Acidification: The Other CO2 Problem. ''Annu. Rev. Mar. Sci. 1:169–92''</ref>		“Rising atmospheric carbon dioxide (CO2) is one of the most critical problems because its effects are globally pervasive and irreversible on ecological timescales. The primary direct consequences are increasing ocean temperatures <ref> Bindoff, N.L., J. Willebrand, V. Artale, A, Cazenave, J. Gregory, S. Gulev, K. Hanawa, C. Le Quéré, S. Levitus, Y. Nojiri, C.K. Shum, L.D. Talley and A. Unnikrishnan, 2007: Observations: Oceanic Climate Change and Sea Level. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA </ref> and acidity <ref>[https://imedea.uib-csic.es/master/cambioglobal/Modulo_III_cod101608/Tema_8-acidificación/pH/annurev.marine.010908.163834.pdf] Doney,S. C., Fabry, V. J., Feely, R. A. and Kleypas J. A. (2009) Ocean Acidification: The Other CO2 Problem. ''Annu. Rev. Mar. Sci. 1:169–92''</ref>.

	Climbing temperatures create a host of additional changes, such as rising sea level, increased ocean stratification, decreased sea-ice extent, and altered patterns of ocean circulation, precipitation, and freshwater input. In addition, both warming and altered ocean circulation act to reduce subsurface oxygen (O2) concentrations <ref> Keeling, R. E., Kortzinger, A. and Gruber, N. (2010), Ocean deoxygenation in a warming world, Annu. Rev. Mar. Sci., 2, 199–229, doi:10.1146/annurev .marine.010908.163855.</ref> In recent decades, the rates of change have been rapid and may exceed the current and potential future tolerances of many organisms to adapt. Further, the rates of physical and chemical change in marine ecosystems will almost certainly accelerate over the next several decades in the absence of immediate and dramatic efforts toward climate mitigation.”		Climbing temperatures create a host of additional changes, such as rising sea level, increased ocean stratification, decreased sea-ice extent, and altered patterns of ocean circulation, precipitation, and freshwater input. In addition, both warming and altered ocean circulation act to reduce subsurface oxygen (O2) concentrations <ref> Keeling, R. E., Kortzinger, A. and Gruber, N. (2010), Ocean deoxygenation in a warming world, Annu. Rev. Mar. Sci., 2, 199–229, doi:10.1146/annurev .marine.010908.163855.</ref> In recent decades, the rates of change have been rapid and may exceed the current and potential future tolerances of many organisms to adapt. Further, the rates of physical and chemical change in marine ecosystems will almost certainly accelerate over the next several decades in the absence of immediate and dramatic efforts toward climate mitigation.”

Youarethecause: /* See also... */

2018-07-11T13:30:34Z

Youarethecause at 13:30, 11 July 2018

2018-07-11T13:30:04Z

← Older revision		Revision as of 13:30, 11 July 2018
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	“Rising atmospheric carbon dioxide (CO2) is one of the most critical problems because its effects are globally pervasive and irreversible on ecological timescales ~~(Natl. Res. Counc. 2011)~~. The primary direct consequences are increasing ocean temperatures <ref> Bindoff, N.L., J. Willebrand, V. Artale, A, Cazenave, J. Gregory, S. Gulev, K. Hanawa, C. Le Quéré, S. Levitus, Y. Nojiri, C.K. Shum, L.D. Talley and A. Unnikrishnan, 2007: Observations: Oceanic Climate Change and Sea Level. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA </ref> and acidity. <ref>[https://imedea.uib-csic.es/master/cambioglobal/Modulo_III_cod101608/Tema_8-acidificación/pH/annurev.marine.010908.163834.pdf] Doney,S. C., Fabry, V. J., Feely, R. A. and Kleypas J. A. (2009) Ocean Acidification: The Other CO2 Problem. ''Annu. Rev. Mar. Sci. 1:169–92''</ref>		“Rising atmospheric carbon dioxide (CO2) is one of the most critical problems because its effects are globally pervasive and irreversible on ecological timescales. The primary direct consequences are increasing ocean temperatures <ref> Bindoff, N.L., J. Willebrand, V. Artale, A, Cazenave, J. Gregory, S. Gulev, K. Hanawa, C. Le Quéré, S. Levitus, Y. Nojiri, C.K. Shum, L.D. Talley and A. Unnikrishnan, 2007: Observations: Oceanic Climate Change and Sea Level. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA </ref> and acidity. <ref>[https://imedea.uib-csic.es/master/cambioglobal/Modulo_III_cod101608/Tema_8-acidificación/pH/annurev.marine.010908.163834.pdf] Doney,S. C., Fabry, V. J., Feely, R. A. and Kleypas J. A. (2009) Ocean Acidification: The Other CO2 Problem. ''Annu. Rev. Mar. Sci. 1:169–92''</ref>

	Climbing temperatures create a host of additional changes, such as rising sea level, increased ocean stratification, decreased sea-ice extent, and altered patterns of ocean circulation, precipitation, and freshwater input. In addition, both warming and altered ocean circulation act to reduce subsurface oxygen (O2) concentrations <ref> Keeling, R. E., Kortzinger, A. and Gruber, N. (2010), Ocean deoxygenation in a warming world, Annu. Rev. Mar. Sci., 2, 199–229, doi:10.1146/annurev .marine.010908.163855.</ref> In recent decades, the rates of change have been rapid and may exceed the current and potential future tolerances of many organisms to adapt. Further, the rates of physical and chemical change in marine ecosystems will almost certainly accelerate over the next several decades in the absence of immediate and dramatic efforts toward climate mitigation.”		Climbing temperatures create a host of additional changes, such as rising sea level, increased ocean stratification, decreased sea-ice extent, and altered patterns of ocean circulation, precipitation, and freshwater input. In addition, both warming and altered ocean circulation act to reduce subsurface oxygen (O2) concentrations <ref> Keeling, R. E., Kortzinger, A. and Gruber, N. (2010), Ocean deoxygenation in a warming world, Annu. Rev. Mar. Sci., 2, 199–229, doi:10.1146/annurev .marine.010908.163855.</ref> In recent decades, the rates of change have been rapid and may exceed the current and potential future tolerances of many organisms to adapt. Further, the rates of physical and chemical change in marine ecosystems will almost certainly accelerate over the next several decades in the absence of immediate and dramatic efforts toward climate mitigation.”

Youarethecause at 13:27, 11 July 2018

2018-07-11T13:27:46Z

← Older revision		Revision as of 13:27, 11 July 2018
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	“Rising atmospheric carbon dioxide (CO2) is one of the most critical problems because its effects are globally pervasive and irreversible on ecological timescales (Natl. Res. Counc. 2011). The primary direct consequences are increasing ocean temperatures <ref> Bindoff, N.L., J. Willebrand, V. Artale, A, Cazenave, J. Gregory, S. Gulev, K. Hanawa, C. Le Quéré, S. Levitus, Y. Nojiri, C.K. Shum, L.D. Talley and A. Unnikrishnan, 2007: Observations: Oceanic Climate Change and Sea Level. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA </ref> and acidity. <[https://imedea.uib-csic.es/master/cambioglobal/Modulo_III_cod101608/Tema_8-acidificación/pH/annurev.marine.010908.163834.pdf] Doney,S. C., Fabry, V. J., Feely, R. A. and Kleypas J. A. (2009) Ocean Acidification: The Other CO2 Problem. ''Annu. Rev. Mar. Sci. 1:169–92''</ref>		“Rising atmospheric carbon dioxide (CO2) is one of the most critical problems because its effects are globally pervasive and irreversible on ecological timescales (Natl. Res. Counc. 2011). The primary direct consequences are increasing ocean temperatures <ref> Bindoff, N.L., J. Willebrand, V. Artale, A, Cazenave, J. Gregory, S. Gulev, K. Hanawa, C. Le Quéré, S. Levitus, Y. Nojiri, C.K. Shum, L.D. Talley and A. Unnikrishnan, 2007: Observations: Oceanic Climate Change and Sea Level. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA </ref> and acidity. <ref>[https://imedea.uib-csic.es/master/cambioglobal/Modulo_III_cod101608/Tema_8-acidificación/pH/annurev.marine.010908.163834.pdf] Doney,S. C., Fabry, V. J., Feely, R. A. and Kleypas J. A. (2009) Ocean Acidification: The Other CO2 Problem. ''Annu. Rev. Mar. Sci. 1:169–92''</ref>

	Climbing temperatures create a host of additional changes, such as rising sea level, increased ocean stratification, decreased sea-ice extent, and altered patterns of ocean circulation, precipitation, and freshwater input. In addition, both warming and altered ocean circulation act to reduce subsurface oxygen (O2) concentrations <ref> Keeling, R. E., Kortzinger, A. and Gruber, N. (2010), Ocean deoxygenation in a warming world, Annu. Rev. Mar. Sci., 2, 199–229, doi:10.1146/annurev .marine.010908.163855.</ref> In recent decades, the rates of change have been rapid and may exceed the current and potential future tolerances of many organisms to adapt. Further, the rates of physical and chemical change in marine ecosystems will almost certainly accelerate over the next several decades in the absence of immediate and dramatic efforts toward climate mitigation.”		Climbing temperatures create a host of additional changes, such as rising sea level, increased ocean stratification, decreased sea-ice extent, and altered patterns of ocean circulation, precipitation, and freshwater input. In addition, both warming and altered ocean circulation act to reduce subsurface oxygen (O2) concentrations <ref> Keeling, R. E., Kortzinger, A. and Gruber, N. (2010), Ocean deoxygenation in a warming world, Annu. Rev. Mar. Sci., 2, 199–229, doi:10.1146/annurev .marine.010908.163855.</ref> In recent decades, the rates of change have been rapid and may exceed the current and potential future tolerances of many organisms to adapt. Further, the rates of physical and chemical change in marine ecosystems will almost certainly accelerate over the next several decades in the absence of immediate and dramatic efforts toward climate mitigation.”

Youarethecause at 13:27, 11 July 2018

2018-07-11T13:27:11Z

← Older revision		Revision as of 13:27, 11 July 2018
Line 1:		Line 1:
	“Rising atmospheric carbon dioxide (CO2) is one of the most critical problems because its effects are globally pervasive and irreversible on ecological timescales (Natl. Res. Counc. 2011). The primary direct consequences are increasing ocean temperatures <ref> Bindoff, N.L., J. Willebrand, V. Artale, A, Cazenave, J. Gregory, S. Gulev, K. Hanawa, C. Le Quéré, S. Levitus, Y. Nojiri, C.K. Shum, L.D. Talley and A. Unnikrishnan, 2007: Observations: Oceanic Climate Change and Sea Level. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA and acidity. <[https://imedea.uib-csic.es/master/cambioglobal/Modulo_III_cod101608/Tema_8-acidificación/pH/annurev.marine.010908.163834.pdf] Doney,S. C., Fabry, V. J., Feely, R. A. and Kleypas J. A. (2009) Ocean Acidification: The Other CO2 Problem. ''Annu. Rev. Mar. Sci. 1:169–92''</ref>		“Rising atmospheric carbon dioxide (CO2) is one of the most critical problems because its effects are globally pervasive and irreversible on ecological timescales (Natl. Res. Counc. 2011). The primary direct consequences are increasing ocean temperatures <ref> Bindoff, N.L., J. Willebrand, V. Artale, A, Cazenave, J. Gregory, S. Gulev, K. Hanawa, C. Le Quéré, S. Levitus, Y. Nojiri, C.K. Shum, L.D. Talley and A. Unnikrishnan, 2007: Observations: Oceanic Climate Change and Sea Level. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA </ref> and acidity. <[https://imedea.uib-csic.es/master/cambioglobal/Modulo_III_cod101608/Tema_8-acidificación/pH/annurev.marine.010908.163834.pdf] Doney,S. C., Fabry, V. J., Feely, R. A. and Kleypas J. A. (2009) Ocean Acidification: The Other CO2 Problem. ''Annu. Rev. Mar. Sci. 1:169–92''</ref>

	Climbing temperatures create a host of additional changes, such as rising sea level, increased ocean stratification, decreased sea-ice extent, and altered patterns of ocean circulation, precipitation, and freshwater input. In addition, both warming and altered ocean circulation act to reduce subsurface oxygen (O2) concentrations <ref> Keeling, R. E., Kortzinger, A. and Gruber, N. (2010), Ocean deoxygenation in a warming world, Annu. Rev. Mar. Sci., 2, 199–229, doi:10.1146/annurev .marine.010908.163855.</ref> In recent decades, the rates of change have been rapid and may exceed the current and potential future tolerances of many organisms to adapt. Further, the rates of physical and chemical change in marine ecosystems will almost certainly accelerate over the next several decades in the absence of immediate and dramatic efforts toward climate mitigation.”		Climbing temperatures create a host of additional changes, such as rising sea level, increased ocean stratification, decreased sea-ice extent, and altered patterns of ocean circulation, precipitation, and freshwater input. In addition, both warming and altered ocean circulation act to reduce subsurface oxygen (O2) concentrations <ref> Keeling, R. E., Kortzinger, A. and Gruber, N. (2010), Ocean deoxygenation in a warming world, Annu. Rev. Mar. Sci., 2, 199–229, doi:10.1146/annurev .marine.010908.163855.</ref> In recent decades, the rates of change have been rapid and may exceed the current and potential future tolerances of many organisms to adapt. Further, the rates of physical and chemical change in marine ecosystems will almost certainly accelerate over the next several decades in the absence of immediate and dramatic efforts toward climate mitigation.”
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	[[Category:Marine Related Issues]]		[[Category:Marine Related Issues]]
	[[[[Category:EU Marine Directives]]		[[[[Category:EU Marine Directives]]

	~~==References==~~

	==References==		==References==

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2018-07-11T13:25:09Z

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“Rising atmospheric carbon dioxide (CO2) is one of the most critical problems because its effects are globally pervasive and irreversible on ecological timescales (Natl. Res. Counc. 2011). The primary direct consequences are increasing ocean temperatures <ref> Bindoff, N.L., J. Willebrand, V. Artale, A, Cazenave, J. Gregory, S. Gulev, K. Hanawa, C. Le Quéré, S. Levitus, Y. Nojiri, C.K. Shum, L.D. Talley and A. Unnikrishnan, 2007: Observations: Oceanic Climate Change and Sea Level. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA and acidity. <[https://imedea.uib-csic.es/master/cambioglobal/Modulo_III_cod101608/Tema_8-acidificación/pH/annurev.marine.010908.163834.pdf] Doney,S. C., Fabry, V. J., Feely, R. A. and Kleypas J. A. (2009) Ocean Acidification: The Other CO2 Problem. ''Annu. Rev. Mar. Sci. 1:169–92''</ref>

Climbing temperatures create a host of additional changes, such as rising sea level, increased ocean stratification, decreased sea-ice extent, and altered patterns of ocean circulation, precipitation, and freshwater input. In addition, both warming and altered ocean circulation act to reduce subsurface oxygen (O2) concentrations <ref> Keeling, R. E., Kortzinger, A. and Gruber, N. (2010), Ocean deoxygenation in a warming world, Annu. Rev. Mar. Sci., 2, 199–229, doi:10.1146/annurev .marine.010908.163855.</ref> In recent decades, the rates of change have been rapid and may exceed the current and potential future tolerances of many organisms to adapt. Further, the rates of physical and chemical change in marine ecosystems will almost certainly accelerate over the next several decades in the absence of immediate and dramatic efforts toward climate mitigation.”

==See also...==
[[Climate Change]]
[[Category:Marine Related Issues]]
[[[[Category:EU Marine Directives]]

==References==

==References==

← Older revision		Revision as of 13:30, 11 July 2018
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	[[Climate Change]]		[[Climate Change]]
	[[Category:Marine Related Issues]]		[[Category:Marine Related Issues]]
	[[[[Category:EU Marine Directives]]		[[Category:EU Marine Directives]]

	==References==		==References==