Differences

This shows you the differences between two versions of the page.

--- pmip3:wg:p2f:data [2013/12/03 16:43] – [The Eocene] lunt
+++ pmip3:wg:p2f:data [2017/02/28 10:16] (current) – [The Pliocene] jules
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 More details: https://www.dokuwiki.org/plugin:discussion */
 ~~DISCUSSION~~
-Contact  --- //[[valerie.masson@lsce.ipsl.fr|Valérie Masson-Delmotte]] 2013/04/26 06:53// to contribute to this page, or leave a comment in the discussion box.
+Contact  --- //[[jules@blueskiesresearch.org.uk|Julia Hargreaves]] 2013/04/26 06:53// to contribute to this page, or leave a comment in the discussion box.
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 /* Title of the page... :-) */
-====== New PMIP3 page template ======
+====== How to find actual data to compare to model output ======
-<note info>PAGE under construction!!!</note>
+I am sure there is more than indicated below. Ask the authors of [[pmip3:wg:p2f:models|the Experimental description papers]]!
-===== Links to data, grouped by PMIP interval =====
 ==== Last one or two millennia ====
 ==== mid-Holocene - 6ka ====
+Land, pollen data. [[pmip3:synth:bartlein:index|Continental climate reconstructions for mid-Holocene and Last Glacial Maximum]]\\ (Bartlein et al, 2011)
 ==== 8.5kyear event (?) ====
 ==== The last deglaciation/termination ====
+[[pmip3:synth:bartlein:index|Continental climate reconstructions for mid-Holocene and Last Glacial Maximum]]\\ (Bartlein et al, 2011)
 ==== The Last Glacial Maximum ====
+[[pmip3:synth:dinezio:index|Indo-Pacific Last Glacial Maximum hydroclimate proxy synthesis ]]\\ (DiNezio and Tierney, 2013)
+SST, multi proxy. [[http://margo.pangaea.de/|Multiproxy Approach for the Reconstruction of the Glacial Ocean surface]]\\ (MARGO)
+Land, pollen data. [[pmip3:synth:bartlein:index|Continental climate reconstructions for mid-Holocene and Last Glacial Maximum]]\\ (Bartlein et al, 2011)
 ==== The Eemian ====
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 ==== The Pliocene ====
+Harry Dowsett is working on the new Prism4 SST synthesis for the PlioMIP2 project. It will be published in a USGS publication - currently still in progress (as of February 2017).
+There is also SST from PRISM3 (2010). The data for PRISM3 were drawn from various warm periods about 3Ma. Thus they do not present a single consistent climate snapshot of the kind that may be produced by a climate model. These data were used in PlioMIP1. See, for example, this paper comparing PRISM3 and the model HadCM3 and references therein. http://www.sciencedirect.com/science/article/pii/S0031018211001404
 ==== The Eocene ====