*-----------------------------------------------------------------------------------------
* SST_SSS_DIFF_xy_JUL_yr2080-2070_Indo.ps
  Six figs of SST and SSS are put together in this file:

(a)  SST_NEMO_JUL2007_Indo.eps
(b)  SST_2XCO2_Scenario_2L23B_JUL2080_Indo.eps
(c)  SST_Diff_2XCO2_Scenario_2L23B_JUL2080-NEMO_JUL2007_Indo.eps
  and
(d)  SSS_NEMO_JUL2007_Indo.eps
(e)  SSS_2XCO2_Scenario_2L23B_JUL2080_Indo.eps
(f)  SSS_Diff_2XCO2_Scenario_2L23B_JUL2080-NEMO_JUL2007_Indo.eps

  (a), (b), (c): SST increases in the entire Indian Ocean. In particular, the increases
  in the Arabian Sea along the coast lines of the Arabian Peninsula, Horn of Africa and
  the northwest coast in the Bay of Bengal reach as much as 6 deg C.

  (d), (e), (f): Inceases in SSS are found in the most region of the Arabian Sea and
  in the ocean south of 20S. SSS decreases are found the
  rest of the Indian Ocean. Particularly, the SST decrease reaches ~2 psu in the Bay of 
  Bengal.

*-----------------------------------------------------------------------------------------
* CHL_PPPHY_DIFF_xy_yr2080-2070_Indo.ps
  Six figs of Nano and diatoms chlorophyl concentrations (NCHL and DCHL) and
  primary production of nanophytoplankton (PPPHY) and primary production of 
  diatoms (PPPHY2) are put together in this file:

(a)  NCHL+DCHL_NEMO_JUL2007_Indo.eps
(b)  NCHL+DCHL_2XCO2_Scenario_2L23B_JUL2080_Indo.eps
(c)  NCHL+DCHL_Diff_2XCO2_Scenario_2L23B_JUL2080-NEMO_JUL2007_Indo.eps
     and
(d)  PPPHY+PPPHY2_NEMO_2007_Indo.eps
(e)  PPPHY+PPPHY2_2XCO2_Scenario_2L23B_2080_Indo.eps
(f)  PPPHY+PPPHY2_Diff_2XCO2_Scenario_2L23B_2080-NEMO_2007_Indo.eps

  (a), (b), (c): The chlorophyl concentrations (sum of NCHL and DCHL) in the top 30 m of 
  the surface ocean become smaller 
  in general, particurally in the Arabian Sea along the coast lines of the Arabian
  Peninsula, Horn of Africa, and around Sri Lanka. Weak increases occur in the southern 
  ocean and in the Bay of Bengal.

  (d), (e), (f): Primary productions (sum of PPPHY and PPPHY2) in the top 30 m of 
  the surface ocean decrease in the regions
  where the decrease of chlorophyl concentrations are observed. Increases are found along 
  the northern and eastern coastal region of the Arabian Sea and in the most area in 
  the Bay of Bengal.

*-----------------------------------------------------------------------------------------
* MLD_DpCO2_DIFFxy_yr2080-2070_Indo.ps
  Six figs of Mixed layer depth (MLD) and delta pCO2 (air-seawater, DpCO2) are put 
  together in this file: 

(a)  MLD_NEMO_JUL2007_Indo.eps
(b)  MLD_2XCO2_Scenario_2L23B_JUL2080_Indo.eps
(c)  MLD_Diff_2XCO2_Scenario_2L23B_JUL2080-NEMO_JUL2007_Indo.eps
     and
(d)  DpCO2_NEMO_2007_Indo.eps
(e)  DpCO2_2XCO2_Scenario_2L23B_2080_Indo.eps
(f)  DpCO2_Diff_2XCO2_Scenario_2L23B_2080-NEMO_2007_Indo.eps

  (a), (b), (c): The MLD becomes shallower in general except in some patched regions 
  along the coasts and in the wide area along 25S from 40E to 90E where the MLD is
  increases.

  The negative values in (d) and (e) indicate that the ocean is a source for atmospheric 
  CO2, and the positive values indicate CO2 sinks. (f) indicates DpCO2 increases in a 
  majority reagion of the Indian Ocean, especially in the Arabian Sea to become
  a weaker source for atmospheric CO2. In the ocean south of 15S the CO2 sink in the 
  eastern region becomes enhanced while it appears to become weaker in the western region.

*-----------------------------------------------------------------------------------------
*IPCC_2007_fig3-2.eps
  Figure 3.2. adopted from IPCC (2007) showing surface warming for the SRES scenarios 
  A2, A1B and B1.

  Left panel: Solid lines are multi-model global averages of surface warming 
  (relative to 1980-1999) for the SRES scenarios A2, A1B and B1,
  shown as continuations of the 20th century simulations. 
  The orange line is for the experiment where concentrations were held constant at year 
  2000 values. The bars in the middle of the figure indicate the best estimate 
  (solid line within each bar) and the likely range assessed for the six SRES marker 
  scenarios at 2090-2099 relative to 1980-1999. The assessment of the best estimate and 
  likely ranges in the bars includes the Atmosphere-Ocean General Circulation Models 
  (AOGCMs) in the left part of the figure, as well as results from a hierarchy of 
  independent models and observational constraints.

  Right panels: Projected surface temperature changes for the early and late 21st century 
  relative to the period 1980-1999. The panels show the multi-AOGCM
  average projections for the A2 (top), A1B (middle) and B1 (bottom) SRES scenarios 
  averaged over decades 2020-2029 (left) and 2090-2099 (right). 

*-----------------------------------------------------------------------------------------
*ipcc_ddc_co2_scenarios.eps
  Figure 1 adopted from IPCC (2007) showing atmospheric CO2 concentrations
  for the SRES scenarios.

  Atmospheric CO2 concentrations as observed at Mauna Loa from 
  1958 to 2008 (black dashed line) and projected under the 6 SRES marker and 
  illustrative scenarios. Two carbon cycle models (see Box 3.7 in IPCC, 2001) 
  are used for each scenario: BERN (solid lines) and ISAM (dashed).