pmip3:wg:degla:bc:ice
Differences
This shows you the differences between two versions of the page.
| Both sides previous revision Previous revision Next revision | Previous revision Next revision Both sides next revision | ||
|
pmip3:wg:degla:bc:ice [2015/02/18 17:22] ruza [Foreword] |
pmip3:wg:degla:bc:ice [2015/03/02 10:17] ruza [Sea Level Equivalent (SLE)] |
||
|---|---|---|---|
| Line 5: | Line 5: | ||
| More info here: http://wiki.splitbrain.org/plugin:discussion */ | More info here: http://wiki.splitbrain.org/plugin:discussion */ | ||
| - | /* ~~DISCUSSION|Discussion on core experiment design~~ * | + | ~~DISCUSSION|Discussion on core experiment design~~ |
| ====== Last Deglaciation Ice Sheets ====== | ====== Last Deglaciation Ice Sheets ====== | ||
| Line 13: | Line 13: | ||
| [[pmip3:wg:degla:bc:core|Go back]] to the main core experiment design page. \\ | [[pmip3:wg:degla:bc:core|Go back]] to the main core experiment design page. \\ | ||
| [[pmip3:wg:degla:index|Go back]] to the main working group page. \\ | [[pmip3:wg:degla:index|Go back]] to the main working group page. \\ | ||
| - | Please note, this page is a work in progress and is not ready for discussion yet. \\ | ||
| \\ | \\ | ||
| Please use the //Discussion// section below to specifically comment on the choice of __ice sheet reconstructions__ for the core experiment. | Please use the //Discussion// section below to specifically comment on the choice of __ice sheet reconstructions__ for the core experiment. | ||
| Line 56: | Line 55: | ||
| The information in this section was provided directly by Dick Peltier et al., October 2014: | The information in this section was provided directly by Dick Peltier et al., October 2014: | ||
| - | > Time dependent //ice-equivalent// contribution to eustatic sea level rise [relative to present day] from each of the primary geographical regions from which grounded ice loss occurred during the [last] deglaciation process. ((Plot provided by Dick Peltier, October 2014)) {{ http://homepages.see.leeds.ac.uk/~earri/pmip_deglac/ICE-6GC_ESL.png?400 |ICE-6G_C Eustatic Sea Level Equivalent of ice volume }} | + | > Time dependent //ice-equivalent// contribution to eustatic sea level rise [relative to present day] from each of the primary geographical regions from which grounded ice loss occurred during the [last] deglaciation process. ((Plot provided by Dick Peltier, October 2014)) {{ http://homepages.see.leeds.ac.uk/~earri/pmip_deglac/ICE-6GC_ESL.png?500 |ICE-6G_C Eustatic Sea Level Equivalent of ice volume }} |
| ^ Ice-equivalent contribution to eustatic sea level rise (m) ((relative to present day and assuming ocean area = 360,768,600 km<sup>2</sup>)) ^^^^ | ^ Ice-equivalent contribution to eustatic sea level rise (m) ((relative to present day and assuming ocean area = 360,768,600 km<sup>2</sup>)) ^^^^ | ||
| Line 162: | Line 161: | ||
| Please think about the following points and add any comments on these or any other aspects of the experiment design to the discussion section below: [Topics will be added here as they are raised below or by email.] | Please think about the following points and add any comments on these or any other aspects of the experiment design to the discussion section below: [Topics will be added here as they are raised below or by email.] | ||
| * Should ICE-6G_C be provided here in its smoothed format, as offered by Dick Peltier (above; [[pmip3:wg:degla:bc:ice#smoothed_fields]]), its original unsmoothed format, or both? | * Should ICE-6G_C be provided here in its smoothed format, as offered by Dick Peltier (above; [[pmip3:wg:degla:bc:ice#smoothed_fields]]), its original unsmoothed format, or both? | ||
| - | * Should Lev Tarasov's reconstruction be provided with a 500 year timestep? It is currently 1000 years, but can be rerun with a shorter timestep.\\ \\ | + | * Should Lev Tarasov's reconstruction be provided with a 500 year timestep? It is currently 1000 years, but could be provided with a shorter timestep.\\ \\ |
| ---- | ---- | ||
pmip3/wg/degla/bc/ice.txt · Last modified: 2015/10/21 13:49 by ruza
