15.11.2013 Views

Marine Ecosystems Research Department - jamstec japan agency ...

Marine Ecosystems Research Department - jamstec japan agency ...

Marine Ecosystems Research Department - jamstec japan agency ...

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

JAMSTEC 2002 Annual Report<br />

Frontier <strong>Research</strong> System for Global Change<br />

between the older instruments and the modern instruments.<br />

The results of the intercomparison will be used<br />

to improve the -year database of direct, diffuse, and<br />

global radiation under a wide range of synoptic weather<br />

conditions. The global balance of atmospheric CO is<br />

far from equilibrium. The characteristic exchange time<br />

within the atmosphere/ocean/geosphere/biosphere system<br />

is estimated at years. A portion of this<br />

exchange takes place in the Arctic marginal seas, even<br />

in the present of an ice cover. Scientists from the<br />

physics group, together with chemists from the US-<br />

IARC program and researchers from Cold Regions<br />

<strong>Research</strong> and Engineering Laboratory (CRREL), are<br />

investigating the flux of atmospheric CO at the surface<br />

of fast ice. Deal and colleagues have chosen the Bering<br />

and Chukchi Seas as the domain of the ice-oceanecosystem<br />

model they are developing. They will use<br />

this model to improve understanding of how physical<br />

factors (such as retreating sea ice, local climate change)<br />

and biogeochemical changes (such as nutrient levels)<br />

may influence phytoplankton and zooplankton dynamics<br />

and thus DMS dynamics.<br />

<strong>Research</strong> Project for Sustainable Coexistence<br />

of Human, Nature, and the Earth<br />

Ministry of Education, Culture, Sports, Science and<br />

Technology (MEXT) started new strategies to promote<br />

science and technology. The above project is included<br />

in the area of "Environment" as larger new initiative of<br />

the MEXT named "<strong>Research</strong> Revolution <br />

(RR)". The period of the Project is years starting<br />

from Fiscal Year . Among seven subjects of the<br />

Project, FRSGC is responsible in carrying out the<br />

whole or part of the following three subjects.<br />

Subject 1: Future Climate Change Projection using<br />

a High-Resolution Coupled Ocean-Atmosphere<br />

Climate Model<br />

The aim of this project is to conduct a series of<br />

future climate change projection experiments using a<br />

high-resolution coupled ocean-atmosphere climate<br />

model on the Earth Simulator, for reducing and understanding<br />

the uncertainty of the projection. The project<br />

team consists of members of Center for Climate<br />

System <strong>Research</strong> of the University of Tokyo (CCSR),<br />

National Institute for Environmental Studies (NIES),<br />

and Frontier <strong>Research</strong> System for Global Change<br />

(FRSGC), and directed by Prof. Sumi of CCSR. The<br />

climate model used is called MIROC and has been collaboratively<br />

developed by CCSR, NIES and FRSGC.<br />

The project includes the following four subjects:<br />

. Development of a high-resolution coupled oceanatmosphere<br />

climate model<br />

. Designing future climate change projection experiments<br />

based on IPCC SRES scenarios<br />

. Development of component models for the climate<br />

model<br />

. Advancing the climate model of Hadley Centre, UK<br />

Since the members of FRSGC are, in principle,<br />

involved in the first subject, the activity of only that<br />

part is introduced below.<br />

Sub Group for the Development of a High-Resolution<br />

Coupled Ocean-Atmosphere Climate Model<br />

For the high-resolution future climate change projection,<br />

we have targeted the following spatial resolution<br />

of the model:<br />

T spectral truncation (approximately .˚) in<br />

horizontal and levels in vertical for the atmospheric<br />

part<br />

.˚ x .˚ in horizontal and levels in vertical<br />

for the oceanic and sea-ice part<br />

With this atmospheric resolution, regional-scale climatic<br />

features such as Baiu front and tropical cyclones<br />

can be represented. The oceanic resolution should be<br />

higher so that the model can reproduce realistic temporal<br />

variation of sea-surface height and the complex<br />

ocean current system in the northern North Atlantic<br />

and the Arctic Oceans, which is critically important to<br />

reproduce the North Atlantic Deep Water (NADW)<br />

148

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!