Climate Proxy - Revision history

Khider: Add see also

2017-05-01T17:35:05Z

Add see also

Admin at 11:12, 28 April 2017

2017-04-28T11:12:48Z

Khider: Setting categories as ClimateProxy ©

2017-01-25T21:53:26Z

Setting categories as ClimateProxy ©

Jeg at 05:09, 6 September 2016

2016-09-06T05:09:47Z

Khider: Fix broken links

2016-09-04T19:47:14Z

Fix broken links

Khider: Relink marine sediment

2016-06-22T05:36:10Z

Relink marine sediment

Khider: Relink marine sediment

2016-06-22T05:34:56Z

Relink marine sediment

Khider: Change link to marine sediments

2016-06-22T05:34:15Z

Change link to marine sediments

Khider: Create Climate Proxy Page

2016-06-22T05:33:02Z

Create Climate Proxy Page

New page

Climate observations prior to the instrumental era are necessarily indirect. These observations are made on climate '''proxies''' in various geological (e.g. lake or marine sediments, living or fossil coral reefs, cave deposits), glaciological (ice cores or snow pits) or biological (trees) [[archive]]s. Many types of data can often be collected from each archives, each '''sensing''' a different aspect of the environment (sometimes, several aspects at once). A paleoclimate dataset is almost always a [https://en.wikipedia.org/wiki/Time_series time series] of observations made on an archive.

Evans et al. (2013) <ref name="evans2013"> Evans, M. N., Tolwinski-Ward, S. E., Thompson, D. M., & Anchukaitis, K. J. (2013). Applications of proxy system modeling in high resolution paleoclimatology. Quaternary Science Reviews, 76, 16-28. doi:10.1016/j.quascirev.2013.05.024 </ref> define a proxy system as comprised of three components (Fig 1).:

[[File:PSM.jpg|thumb|alt=PSM model from Evans et al. (2013)|Fig. 1: Conceptual generalized proxy system model after Evans et al. (2013) <ref name="evans2013" />. An archive is the medium in which the response of a sensor to environmental forcing in recorded.]]

* The [[sensor]] comprises physical, chemical, and/or biological components that react to environmental conditions. Sensors often respond to more than one environmental [[variable]], and may have complex responses to the environment they sense, including thresholds (record only part of the range of environmental conditions), seasonal biases (record environmental conditions over a few months of the year), and/or nonlinear responses. For instance, [[Foraminifera]] is an often used sensor for oceanic conditions. Multiple observations can be made on this sensor, recording different environmental [[variable]]s. Similarly, picking foraminifera of a given species to conduct the measurements is part of the observation process, though it does affect the sensor definition : the habitat of these forams determines with environmental [[variable]] (e.g. surface, sub-surface, or thermocline temperature) they are most sensitive to.

* The [[archive]] is the medium in which the response of a sensor to environmental forcing is recorded. [[Marine sediment | Marine sediments]] are a type of archive, on which many sensors and observations may be recorded (e.g. Foraminifera Mg/Ca, δ<sup>18</sup>O, <math> U_{37}^{k'} </math>, TEX86)

* [[observation | Observations]] are made on archives and are generally referred to as "proxies". The term "proxy" used ubiquitously, and often ambiguously, throughout the paleoclimate literature, is most commonly equivalent to "sensor + observation". "Observation" is the more explicit, and thus, preferred term, however "proxy" can be treated as a synonym of "observation". For instance, [[Foraminifera Mg/Ca]] is often used to investigate past changes in sea-surface temperature but depends also on sea-surface salinity and deep-ocean carbonate saturation <ref> Khider, D., Huerta, G., Jackson, C., Stott, L. D., & Emile-Geay, J. (2015). A Bayesian, multivariate calibration for Globigerinoides ruber Mg/Ca. Geochemistry Geophysics Geosystems, 16(9), 2916-2932. doi:10.1002/2015GC005844 </ref>. Furthermore, its temperature and salinity dependence is exponential <ref> Anand, P., Elderfield, H., & Conte, M. H. (2003). Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series. Paleoceanography, 18(2), 1050. doi:10.1029/2002PA000846 </ref> <ref> Lea, D. W., Mashiotta, T. A., & Spero, H. J. (1999). Controls on magnesium and strontium uptake in planktonic foraminifera determined by live culturing. Geochimica et cosmochimica acta, 63(16), 2369-2379.
</ref> <ref> Kisakürek, B., Eisenhauer, A., Böhm, F., Garbe-Schönberg, D., & Erez, J. (2008). Controls on shell Mg/Ca and Sr/Ca in cultured planktonic foraminiferan, Globigeriniodes ruber (white). Earth and Planetary Science Letters, 273, 260-269. doi:10.1016/j.epsl.2008.06.026 </ref> while its response to carbonate saturation is thresholded <ref> Regenberg, M., Regenberg, A., Garbe-Schonberg, D., & Lea, D. W. (2014). Global dissolution effects on planktonic foraminiferal Mg/Ca ratios controlled by the calcite-saturation state of bottom waters. Paleoceanography, 29, 127-142. doi:10.1002/2013PA002492 </ref>.

These three major components may be individually modeled, and linked together within a [[Proxy System Model]] <ref name="evans2013" /> <ref> Dee, S., Emile-Geay, J., Evans, M. N., Allam, A., Steig, E. J., & Thompson, D. M. (2015). PRYSM: An open-source framework for PRoxy System Modeling, with applications to oxygen-isotope systems. Journal of Advances in Modeling Earth Systems, 7, 1220-1247. doi:10.1002/2015MS000447
</ref>. Some sensors are common to multiple archives (e.g. δ<sup>18</sup>O), and all archives support more than one possible sensor.

==References==
<references />

← Older revision		Revision as of 17:35, 1 May 2017
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	Climate observations prior to the instrumental era are necessarily indirect. These observations are made on climate '''proxies''' in various geological (e.g. lake or marine sediments, living or fossil coral reefs, cave deposits), glaciological (ice cores or snow pits) or biological (trees) [[:Category: ProxyArchive © \|archive]]s. Many types of data can often be collected from each archives, each '''sensing''' a different aspect of the environment (sometimes, several aspects at once). A paleoclimate dataset is almost always a [https://en.wikipedia.org/wiki/Time_series time series] of observations made on an archive.		Climate observations prior to the instrumental era are necessarily indirect. These observations are made on climate '''proxies''' in various geological (e.g. lake or marine sediments, living or fossil coral reefs, cave deposits), glaciological (ice cores or snow pits) or biological (trees) [[:Category: ProxyArchive © \|archive]]s. Many types of data can often be collected from each archives, each '''sensing''' a different aspect of the environment (sometimes, several aspects at once). A paleoclimate dataset is almost always a [https://en.wikipedia.org/wiki/Time_series time series] of observations made on an archive.

← Older revision		Revision as of 11:12, 28 April 2017
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−	~~[[Category:ClimateProxy ©]]~~
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	Climate observations prior to the instrumental era are necessarily indirect. These observations are made on climate '''proxies''' in various geological (e.g. lake or marine sediments, living or fossil coral reefs, cave deposits), glaciological (ice cores or snow pits) or biological (trees) [[:Category: ProxyArchive © \|archive]]s. Many types of data can often be collected from each archives, each '''sensing''' a different aspect of the environment (sometimes, several aspects at once). A paleoclimate dataset is almost always a [https://en.wikipedia.org/wiki/Time_series time series] of observations made on an archive.		Climate observations prior to the instrumental era are necessarily indirect. These observations are made on climate '''proxies''' in various geological (e.g. lake or marine sediments, living or fossil coral reefs, cave deposits), glaciological (ice cores or snow pits) or biological (trees) [[:Category: ProxyArchive © \|archive]]s. Many types of data can often be collected from each archives, each '''sensing''' a different aspect of the environment (sometimes, several aspects at once). A paleoclimate dataset is almost always a [https://en.wikipedia.org/wiki/Time_series time series] of observations made on an archive.

← Older revision		Revision as of 21:53, 25 January 2017
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		+	[[Category:ClimateProxy ©]]

	Climate observations prior to the instrumental era are necessarily indirect. These observations are made on climate '''proxies''' in various geological (e.g. lake or marine sediments, living or fossil coral reefs, cave deposits), glaciological (ice cores or snow pits) or biological (trees) [[:Category: ProxyArchive © \|archive]]s. Many types of data can often be collected from each archives, each '''sensing''' a different aspect of the environment (sometimes, several aspects at once). A paleoclimate dataset is almost always a [https://en.wikipedia.org/wiki/Time_series time series] of observations made on an archive.		Climate observations prior to the instrumental era are necessarily indirect. These observations are made on climate '''proxies''' in various geological (e.g. lake or marine sediments, living or fossil coral reefs, cave deposits), glaciological (ice cores or snow pits) or biological (trees) [[:Category: ProxyArchive © \|archive]]s. Many types of data can often be collected from each archives, each '''sensing''' a different aspect of the environment (sometimes, several aspects at once). A paleoclimate dataset is almost always a [https://en.wikipedia.org/wiki/Time_series time series] of observations made on an archive.

@@ Line 4: / Line 4: @@
 Evans et al. (2013) <ref name="evans2013"> Evans, M. N., Tolwinski-Ward, S. E., Thompson, D. M., & Anchukaitis, K. J. (2013). Applications of proxy system modeling in high resolution paleoclimatology. Quaternary Science Reviews, 76, 16-28. doi:10.1016/j.quascirev.2013.05.024 </ref> define a proxy system as comprised of three components (Fig 1).:
-[[File:PSM.jpg|thumb|alt=PSM model from Evans et al. (2013)|Fig. 1: Conceptual generalized proxy system model after Evans et al. (2013) <ref name="evans2013" />. An archive is the medium in which the response of a sensor to environmental forcing in recorded.]]
+[[File:PSM.jpg|thumb|alt=PSM model from Evans et al. (2013)|Fig. 1: Conceptual proxy system model, after Evans et al. (2013) <ref name="evans2013" />. An archive is the medium in which the response of a sensor to environmental forcing in recorded.]]
 * The [[:Category: ProxySensor  ©| sensor]] comprises physical, chemical, and/or biological components that react to environmental conditions. Sensors often respond to more than one environmental [[variable]], and may have complex responses to the environment they sense, including thresholds  (record only part of the range of environmental conditions), seasonal biases (record environmental conditions over a few months of the year), and/or  nonlinear responses. For instance, [[:Category:Foraminifera | foraminifera]] are an often used sensor for oceanic conditions. Multiple observations can be made on this sensor, recording different environmental [[variable]]s. Similarly, picking foraminifera of a given species to conduct the measurements is part of the observation process, though it does affect the sensor definition : the habitat of these forams determines with environmental [[variable]] (e.g. surface, sub-surface, or thermocline temperature) they are most sensitive to.

@@ Line 1: / Line 1: @@
-Climate observations prior to the instrumental era are necessarily indirect. These observations are made on climate '''proxies''' in various geological (e.g. lake or marine sediments, living or fossil coral reefs, cave deposits), glaciological (ice cores or snow pits) or biological (trees) [[archive]]s. Many types of data can often be collected from each archives, each '''sensing''' a different aspect of the environment (sometimes, several aspects at once).  A paleoclimate dataset is almost always a [https://en.wikipedia.org/wiki/Time_series time series] of observations made on an archive.
+Climate observations prior to the instrumental era are necessarily indirect. These observations are made on climate '''proxies''' in various geological (e.g. lake or marine sediments, living or fossil coral reefs, cave deposits), glaciological (ice cores or snow pits) or biological (trees) [[:Category: ProxyArchive © |archive]]s. Many types of data can often be collected from each archives, each '''sensing''' a different aspect of the environment (sometimes, several aspects at once).  A paleoclimate dataset is almost always a [https://en.wikipedia.org/wiki/Time_series time series] of observations made on an archive.
 Evans et al. (2013) <ref name="evans2013"> Evans, M. N., Tolwinski-Ward, S. E., Thompson, D. M., & Anchukaitis, K. J. (2013). Applications of proxy system modeling in high resolution paleoclimatology. Quaternary Science Reviews, 76, 16-28. doi:10.1016/j.quascirev.2013.05.024 </ref> define a proxy system as comprised of three components (Fig 1).:
@@ Line 6: / Line 6: @@
 [[File:PSM.jpg|thumb|alt=PSM model from Evans et al. (2013)|Fig. 1: Conceptual generalized proxy system model after Evans et al. (2013) <ref name="evans2013" />. An archive is the medium in which the response of a sensor to environmental forcing in recorded.]]
-* The [[sensor]] comprises physical, chemical, and/or biological components that react to environmental conditions. Sensors often respond to more than one environmental [[variable]], and may have complex responses to the environment they sense, including thresholds  (record only part of the range of environmental conditions), seasonal biases (record environmental conditions over a few months of the year), and/or  nonlinear responses. For instance, [[Foraminifera]] is an often used sensor for oceanic conditions. Multiple observations can be made on this sensor, recording different environmental [[variable]]s. Similarly, picking foraminifera of a given species to conduct the measurements is part of the observation process, though it does affect the sensor definition : the habitat of these forams determines with environmental [[variable]] (e.g. surface, sub-surface, or thermocline temperature) they are most sensitive to.
+* The [[:Category: ProxySensor  ©| sensor]] comprises physical, chemical, and/or biological components that react to environmental conditions. Sensors often respond to more than one environmental [[variable]], and may have complex responses to the environment they sense, including thresholds  (record only part of the range of environmental conditions), seasonal biases (record environmental conditions over a few months of the year), and/or  nonlinear responses. For instance, [[:Category:Foraminifera | foraminifera]] are an often used sensor for oceanic conditions. Multiple observations can be made on this sensor, recording different environmental [[variable]]s. Similarly, picking foraminifera of a given species to conduct the measurements is part of the observation process, though it does affect the sensor definition : the habitat of these forams determines with environmental [[variable]] (e.g. surface, sub-surface, or thermocline temperature) they are most sensitive to.
-* The [[archive]] is the medium in which the response of a sensor to environmental forcing is recorded. [[Marine Sediment | Marine Sediments]] are a type of archive, on which many sensors and observations may be recorded (e.g. Foraminifera Mg/Ca, &delta;<sup>18</sup>O, <math> U_{37}^{k'} </math>, TEX86)
+* The [[:Category:ProxyArchive ©| archive]] is the medium in which the response of a sensor to environmental forcing is recorded. [[:Category:MarineSediment | Marine sediments]] are a type of archive, on which many sensors and observations may be recorded (e.g. Foraminifera Mg/Ca, &delta;<sup>18</sup>O, <math> U_{37}^{k'} </math>, TEX86)
-* [[observation | Observations]] are made on archives and are  generally referred to as "proxies". The term "proxy" used ubiquitously, and often ambiguously, throughout the paleoclimate literature, is most commonly equivalent to "sensor + observation". "Observation" is the more explicit, and thus, preferred term, however "proxy" can be treated as a synonym of "observation". For instance, [[Foraminifera Mg/Ca]] is often used to investigate past changes in sea-surface temperature but depends also on sea-surface salinity and deep-ocean carbonate saturation <ref> Khider, D., Huerta, G., Jackson, C., Stott, L. D., & Emile-Geay, J. (2015). A Bayesian, multivariate calibration for Globigerinoides ruber Mg/Ca. Geochemistry Geophysics Geosystems, 16(9), 2916-2932. doi:10.1002/2015GC005844 </ref>.  Furthermore, its temperature and salinity dependence is exponential <ref> Anand, P., Elderfield, H., & Conte, M. H. (2003). Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series. Paleoceanography, 18(2), 1050. doi:10.1029/2002PA000846 </ref> <ref> Lea, D. W., Mashiotta, T. A., & Spero, H. J. (1999). Controls on magnesium and strontium uptake in planktonic foraminifera determined by live culturing. Geochimica et cosmochimica acta, 63(16), 2369-2379.
+* [[:Category:ProxyObservation ©| Observations]] are made on archives and are  generally referred to as "proxies". The term "proxy" used ubiquitously, and often ambiguously, throughout the paleoclimate literature, is most commonly equivalent to "sensor + observation". "Observation" is the more explicit, and thus, preferred term, however "proxy" can be treated as a synonym of "observation". For instance, [[Foraminifera Mg/Ca]] is often used to investigate past changes in sea-surface temperature but depends also on sea-surface salinity and deep-ocean carbonate saturation <ref> Khider, D., Huerta, G., Jackson, C., Stott, L. D., & Emile-Geay, J. (2015). A Bayesian, multivariate calibration for Globigerinoides ruber Mg/Ca. Geochemistry Geophysics Geosystems, 16(9), 2916-2932. doi:10.1002/2015GC005844 </ref>.  Furthermore, its temperature and salinity dependence is exponential <ref> Anand, P., Elderfield, H., & Conte, M. H. (2003). Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series. Paleoceanography, 18(2), 1050. doi:10.1029/2002PA000846 </ref> <ref> Lea, D. W., Mashiotta, T. A., & Spero, H. J. (1999). Controls on magnesium and strontium uptake in planktonic foraminifera determined by live culturing. Geochimica et cosmochimica acta, 63(16), 2369-2379.
 </ref> <ref> Kisakürek, B., Eisenhauer, A., Böhm, F., Garbe-Schönberg, D., & Erez, J. (2008). Controls on shell Mg/Ca and Sr/Ca in cultured planktonic foraminiferan, Globigeriniodes ruber (white). Earth and Planetary Science Letters, 273, 260-269. doi:10.1016/j.epsl.2008.06.026 </ref> while its response to carbonate saturation is thresholded <ref> Regenberg, M., Regenberg, A., Garbe-Schonberg, D., & Lea, D. W. (2014). Global dissolution effects on planktonic foraminiferal Mg/Ca ratios controlled by the calcite-saturation state of bottom waters. Paleoceanography, 29, 127-142. doi:10.1002/2013PA002492 </ref>.
-These three major components may be individually modeled, and linked together within a [[Proxy System Model]] <ref name="evans2013" /> <ref> Dee, S., Emile-Geay, J., Evans, M. N., Allam, A., Steig, E. J., & Thompson, D. M. (2015). PRYSM: An open-source framework  for PRoxy System Modeling, with applications to oxygen-isotope systems. Journal of Advances in Modeling Earth Systems, 7, 1220-1247. doi:10.1002/2015MS000447
+These three major components may be individually modeled, and linked together within a [[:Category: ProxySystemModel  ©|Proxy System Model]] <ref name="evans2013" /> <ref> Dee, S., Emile-Geay, J., Evans, M. N., Allam, A., Steig, E. J., & Thompson, D. M. (2015). PRYSM: An open-source framework  for PRoxy System Modeling, with applications to oxygen-isotope systems. Journal of Advances in Modeling Earth Systems, 7, 1220-1247. doi:10.1002/2015MS000447
 </ref>. Some sensors are common to multiple archives (e.g. &delta;<sup>18</sup>O), and all archives support more than one possible sensor.

@@ Line 8: / Line 8: @@
 * The [[sensor]] comprises physical, chemical, and/or biological components that react to environmental conditions. Sensors often respond to more than one environmental [[variable]], and may have complex responses to the environment they sense, including thresholds  (record only part of the range of environmental conditions), seasonal biases (record environmental conditions over a few months of the year), and/or  nonlinear responses. For instance, [[Foraminifera]] is an often used sensor for oceanic conditions. Multiple observations can be made on this sensor, recording different environmental [[variable]]s. Similarly, picking foraminifera of a given species to conduct the measurements is part of the observation process, though it does affect the sensor definition : the habitat of these forams determines with environmental [[variable]] (e.g. surface, sub-surface, or thermocline temperature) they are most sensitive to.
-* The [[archive]] is the medium in which the response of a sensor to environmental forcing is recorded. [[Marine sediment | Marine Sediments]] are a type of archive, on which many sensors and observations may be recorded (e.g. Foraminifera Mg/Ca, &delta;<sup>18</sup>O, <math> U_{37}^{k'} </math>, TEX86)
+* The [[archive]] is the medium in which the response of a sensor to environmental forcing is recorded. [[Marine sediment | Marine Sediment]] are a type of archive, on which many sensors and observations may be recorded (e.g. Foraminifera Mg/Ca, &delta;<sup>18</sup>O, <math> U_{37}^{k'} </math>, TEX86)
 * [[observation | Observations]] are made on archives and are  generally referred to as "proxies". The term "proxy" used ubiquitously, and often ambiguously, throughout the paleoclimate literature, is most commonly equivalent to "sensor + observation". "Observation" is the more explicit, and thus, preferred term, however "proxy" can be treated as a synonym of "observation". For instance, [[Foraminifera Mg/Ca]] is often used to investigate past changes in sea-surface temperature but depends also on sea-surface salinity and deep-ocean carbonate saturation <ref> Khider, D., Huerta, G., Jackson, C., Stott, L. D., & Emile-Geay, J. (2015). A Bayesian, multivariate calibration for Globigerinoides ruber Mg/Ca. Geochemistry Geophysics Geosystems, 16(9), 2916-2932. doi:10.1002/2015GC005844 </ref>.  Furthermore, its temperature and salinity dependence is exponential <ref> Anand, P., Elderfield, H., & Conte, M. H. (2003). Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series. Paleoceanography, 18(2), 1050. doi:10.1029/2002PA000846 </ref> <ref> Lea, D. W., Mashiotta, T. A., & Spero, H. J. (1999). Controls on magnesium and strontium uptake in planktonic foraminifera determined by live culturing. Geochimica et cosmochimica acta, 63(16), 2369-2379.