Differences

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--- pmip3:design:8k2:index [2010/03/30 11:37] – renssen
+++ pmip3:design:8k2:index [2010/03/30 13:36] – tarasov
@@ Line 20: / Line 20: @@
 |  Aerosols  |  Same as PI  | |
 |    | |  |
-|  Solar constant  |  xxxx W/m<sup>2</sup>  |  As in PI  |
+|  Solar constant  |  As in PI  |    |
 |  Vegetation     |  prescribed or interactive as in CMIP5 PI  |    |
 |  Ice sheets      |  Remnant Laurentide ice-sheet (provided*)  |  Same as PI  |
@@ Line 34: / Line 34: @@
 **Proposed Background Early Holocene melt-water forcing** (mandatory)
-| Flux      | 0.05 Sv over 500 years |
+| Flux      | 0.05 Sv over 500 years (Geographic routing field will be provided)|
 | Location  | Either part or all of the Labrador Sea (up to the individual modeling groups, as long as it is not added outside the Labrador Sea)|
 **Proposed Lake Agassiz drainage** (mandatory):
-| Fux       | 2.5 Sv over 1 year   |
+| Flux       | 2.5 Sv over 1 year   |
 | Location  | Either part or all of the Labrador Sea (up to the individual modeling groups, as long as it is not added outside the Labrador Sea)|
 | Ensemble  | this experiment should be completed at least three times, beginning at different years in the control simulation|
 | Duration  | experiment should be integrated until the AMOC recovers, except in the case of unrealistically long (i.e., multicentury) recoveries|
 ==== Vegetation ====
@@ Line 54: / Line 51: @@
   * Computed by the model (models with dynamic vegetation)
-There are still questions concerning the possibility to have a 6ka reconstructed vegetation from a combination of model output and data analyses that could be used for sensitivity experiments. Please tell if you are interested by such a map and what would be the best variables (pft?) that should be provided (see comment from B. Otto-Bliesner in the discussion pannel).
-==== For Earth System Models with interactive carbone cycle ====
+==== For Earth System Models with interactive carbon cycle ====
-The simulations are forced by CO2 concentrations. Please use the same protocol as in CMIP5 to store the carbone fluxes and the variables needed for PCMIP (see list here)
+The simulations are forced by CO2 concentrations. Please use the same protocol as in CMIP5 to store the carbon fluxes and the variables needed for PCMIP (see list here)
 ==== Insolation ====