cimp5_2041_2060_ch: Seafloor Climate Change by 2041 to 2060

In chihlinwei/SCC85: Seafloor Climate Change Projections from CIMP5

Seafloor Climate Change by 2041 to 2060

Description

Emsemble average of the decadal mean seafloor (bottom-most) projections during 2041 to 2060 minus the decadal mean projections during 1951 to 2000 based on RCP8.5 scenario of CIMP5 experiment.

Format

A RasterBrick object of 4 raster layers:

epc_av_2041_to_2060_minus_1951_to_2000

Difference in export POC flux to seafloor (mg C m^-2 d^-1)

o2_av_2041_to_2060_minus_1951_to_2000

Difference in dissolved oxygen concentration at seafloor (mol m^-3)

ph_av_2041_to_2060_minus_1951_to_2000

Difference in pH at seafloor

thetao_av_2041_to_2060_minus_1951_to_2000

Difference in potential temperature at seafllor (K)

arag_av_2041_to_2060_minus_1951_to_2000

Difference in aragonite concentration (mol m-3)

calc_av_2041_to_2060_minus_1951_to_2000

Difference in calcite concentration (mol m-3)

co3_av_2041_to_2060_minus_1951_to_2000

Difference in mole concentration of Carbonate expressed as Carbon in Sea Water (mol m-3)

co3satarag_av_2041_to_2060_minus_1951_to_2000

Difference in carbonate ion concentration for seawater in equilibrium with pure aragonite (mol m-3)

co3satcalc_av_2041_to_2060_minus_1951_to_2000

Difference in carbonate ion concentration for seawater in equilibrium with pure calcite (mol m-3)

aragsat_av_2041_to_2060_minus_1951_to_2000

Difference in aragonite Saturation State

calcsat_av_2041_to_2060_minus_1951_to_2000

Difference in calcite Saturation State

Details

Climate change (difference of decadal mean) between the period of 1951 to 2000 and the period 2041 to 2080 were calculated for each of the GFDL-ESM-2G, IPSL-CM5A-MR and MPI-ESM-MR. Emsemble average of climate changes was calculated across the three models.

Source

https://esgf-node.llnl.gov/search/esgf-llnl/

chihlinwei/SCC85 documentation built on Sept. 15, 2023, 4:47 a.m.