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Multimedia
- Film about the CARBOOSCHOOLS project cruise 2006 that took place in Bergen, Norway in a low and in a high resolution
- Short film by Univisjon from the first annual CARBOOCEAN meeting heldt in Amsterdam in November 2005 is available in a low and in a high resolution.
- Short film by Univisjon showing the installation of pCO2 system in available is a low and in a high resolution.
- Film about the 2005 CARBOOCEAN cruise with the R/V Pelagia in a low and a high resolution
- aragonite.m1v: Development of the seawater super saturation for aragonite (the metastable modification of biogenic calcium carbonate along a western Atlantic cross section for an anthropogenic CO2 emission scenario. This emission scenario is comparable to the IPCC SRES A1B (business as usual) scenario and includes historical emissions until 1995, a 1.5%/yr increase until 2030, a slowing increase until 2050 (with peak emissions at year 2050) and a decrease of emissions with 15/yr thereafter. Watch in particular the changes north of 60° north. According to this scenario the high latitude oceans will get undersaturated with respect to aragonite by the end of this century with respective consequences for organisms that produce aragonite shell material. Courtesy of E. Maier-Reimer.
- calcite.m1v: Development of the seawater super saturation for calcite (the more stable modification of biogenic calcium carbonate as compared to aragonite) along a western Atlantic cross section with time for an anthropogenic CO2 emission scenario. This emission scenario is comparable to the IPCC SRES A1B (business as usual) scenario and includes historical emissions until 1995, a 1.5%/yr increase until 2030, a slowing increase until 2050 (with peak emissions at year 2050) and a decrease of emissions with 15/yr thereafter. Watch in particular the changes north of 60° north. Courtesy of E. Maier-Reimer.
- Aragonite_hor_sm.m1v:Development of the seawater super saturation for aragonite the metastable modification of biogenic calcium carbonate in the ocean surface layer for an anthropogenic CO2 emission scenario. This emission scenario is comparable to the IPCC SRES A1B (business as usual) scenario and includes historical emissions until 1995, a 1.5%/yr increase until 2030, a slowing increase until 2050 (with peak emissions at year 2050) and a decrease of emissions with 15/yr thereafter. Watch in particular the changes north of 60° north. Courtesy of E. Maier-Reimer.
- The German channel ARD has recently shown a documentation about the first CARBOOCEAN mesocosm CO2 perturbation study that took place in May / June 2005 in Bergen, Norway. For those of you who were not able to watch the telecast "W - wie Wissen" (July, 20th), the CARBOOCEAN project office will receive a DVD during the next days that can be sent around on request (please contact andrea.volbers@bjerknes.uib.no). Due to legal restrictions we cannot make it available on the internet but we are allowed to use the DVD material for teaching purposes in schools.
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