Report of the conference by Dr. Honda

I attended the Bjerknes Centenary 2004 "Climate Change in High Latitudes" held at Bergen, Norway from 1 to 3, September, 2004. About 300 people, mostly from Europe, attended this conference to present and discuss their latest high-latitude climate studies focusing on the North Atlantic. The main themes of this conference were vertical circulation, carbon circulation, and climate changes in the North Atlantic; and reproduction of palaeoclimate by using high-resolution models, the main research projects of Bjerknes Center for Climate Research, the host of this conference. Many participants made presentations on their own research projects, which was conducted mainly in poster session style. The Center was so overcrowded since number of participants registered for this conference was more than expected.
Through this conference, keen discussions were exchanged. Many FRCGC researchers attended the conference, including Drs. Honda (author) and Takaya from our program. Honda and Takaya made their presentations on studies on climate changes in mid-latitudes regions such as the North Pacific and the Eurasia respectively, while most other presentations were about the climate changes in the North Atlantic regions. In the academic tour of a glacier observation, the participants had detailed explanations about mechanisms of glacier fluctuation, and relationship between the fluctuation and recent global warming, etc. Looking at the decreasing glacier, I could get a real feeling of global warming effect.

Tour participants heading for the glacier as if they were pulled in. (photograph by Dr. Yoshihiro Tachibana, IORGC)

Report of meetings by Dr. Kuba

I stayed at Humburg, Germany for 1 week from 11 July to attend the International Cloud Modeling Workshop 2004. The main purpose of this workshop was to verify models by using data from large-scale observations. At Working Group Meetings, as well as at Plenary Sessions, I was able to have a cooperation from the observation team. After the workshop, I moved to Bologna, Italy to attend the International Conference on Clouds and Precipitation (ICCP2004). The conference was very fulfilling because subjects discussed during the term (1 week) were all related to Cloud Physics. I have worked on determining initial cloud drop size distribution of microphysical model with bin method using the parcel model with particle method in Lagrangian framework form cloud condensation nuclei. However, it is difficult to introduce a parcel model and bin model together into a 3-D nonhydrostatic model. Thus I developed parameterization for determining the initial cloud drop size distribution to introduce at the conference. During discussion among participants, I realized that many researchers had the same problem, and felt sense of solidarity.


Report of a Symposium by Dr. Iwabuchi

I attended the International Radiation Symposium (IRS) 2004 held in Pusan, South Korea for 1 week from 23 August. In this largest international symposium related to Atmospheric Radiation, recent issues in this field were discussed thoroughly. The most impressive presentation was about the study on the regional distribution of radiation balance that is changed by introducing the sub-grid-scale effect of cloud radiation into a global atmospheric circulation. This effect of cloud radiation may also affect other distributions such as precipitation. I then felt the need of introducing this effect into climate models in Japan. Meanwhile, I presented the study on 3-D radiation transfer in atmosphere that includes cloud. Thanks to getting valuable comments from many researchers, I was able to spend fulfilling time in this conference.

Two scientists, Dr. Hitoshi Irie and Dr. Donald Lucas, have joined the Atmospheric Composition Research Program this year. Before this March, Dr. Hitoshi Irie was working at National Institute for Environmental Studies (NIES) to address the issue on the formation process of polar stratospheric clouds, which play a central role in the Arctic ozone depletion, by using satellite data (ADEOS/ILAS) and a cloud microphysics model.
From these experiences, Dr. Irie would like to analyze satellite data at FRCGC to investigate temporal/spatial variations of atmospheric composition and to contribute to solving global environment issues. Dr. Donald Lucas joined our program in May. Dr. Lucas was previously at MIT, where he used a variety of computer models to study the atmospheric chemistry of dimethylsulfide, an important biogenic sulfur compound. At the FRCGC, Dr. Lucas plans to incorporate a size-resolved description of aerosols into a global 3D chemistry-climate model, which he will then use to quantify the production and fate of secondary aerosols in the troposphere.
 
Introduction of Dr. Hideki Kobayashi, who joined the Ecosystem Change Research Program in April 2004

I received doctor's degree in March, 2004. I majored in Material Science in Physics Department at the university, and then studied monitoring methods for land vegetation by using remote sensing in an engineering laboratory of the graduated school. Taking an opportunity to study in a program on ecosystem, I now trying to extent my knowledge. Smoke generated by forest fires in Southeast Asia decreases the amount of photosynthetically available solar radiation and affects the net primary production (NPP) of the plants. In my doctor's course, I evaluated these issues over Southeast Asia using satellite data. Air pollution of East Asia and Southeast Asia is especially serious compared with other regions. Therefore, in the long view, variation of solar radiation environment caused by the air pollution is likely to affect the amount of carbon assimilation of plants. In Ecosystem Change Research Program, I plan to conduct a research on the relationship between the variation of solar radiation and the amount of carbon absorption of plants in whole Asia with Dr. Dennis Dye, the group leader of this program.

Report of the Symposium by Dr. Tsushima

I attended International Radiation Symposium (IRS) held in Pusan, South Korea from 23 to 28 August, 2004, and made a poster presentation. In this symposium, specialists in various fields of Radiation meet once every 4 years. During the poster session, Dr. Wielicki, National Aeronautics and Space Administration (NASA), approached to me and said, "I am going to analyze the same annual variation by using CERES data." I replied willingly, "I want to know if we get the same result with the new data or not. if you conduct the analysis, please tell me the result." At the night banquet, Dr. Ramaswamy, Geophysical Fluid Dynamics Laboratory (GFDL) said to me, "Have you got any advances in analysis of K-1 model of low- and high-sensibility versions?" Indeed, the increased amounts of earth's temperature caused by doubled CO2 that were calculated in models studies at other laboratories are very close; 2.9 degrees in GFDL's model and 2.7degrees in NCAR's model. However, both models showed differences in cloud behavior; lower cloud increases in GFDL's model, but decreases in NCAR's model. There is a strong possibility that the cause of the difference in cloud behavior will be depended on used models, even though both climate resolutions are similar. It is very interesting theme to study the contributions of short-wavelength and long-wavelength radiation to the climate sensitivity as the first stage, and to compare and analyze the cloud feedback mechanisms as the second stage. If the difference of cloud response in warmed models can be related to the difference of cloud distributions and feedback in the models that show present climate, it will be possible to get a clue to identify the causes of global warming resolution's indeterminacy. I am very much looking forward to future studies.

We would like to introduce recent activities of the Next-Generation Model Development Group.

The Atmospheric Modeling subgroup develops a nonhydrostatic and regular icosahedral grid model called NICAM. NICAM, which was installed cloud physical processes and radiation processes already, is scheduled for aqua-planet experiments at a resolution of about 3.5km horizontal grid. The group's goal of this fiscal year is to install an aerosol model to perform experiments such as AMIP-like ones and climate sensibility ones. This group also works on examining non-negative advection, and on examining and improving physical processes (convection parameterization, cloud physical processes, and mixed-layer schemes) on a regular icosahedral grid. The Ocean Modeling subgroup studies the roles of mesoscale eddies, which fill the ocean and rang from several km to several 10 km, in climate system. To identify the mesoscale eddies, it is necessary to cover the whole globe with a fine grid. Therefore, this group works on developing a new mathematically efficient ocean model by using a cubic grid. Now, this group conducts test runs at relatively low-resolution for preparation of future high-resolution climate calculation. Moreover, in cooperation with Center for Climate System Research, University of Tokyo, this group develops local models of the Southern Oceans and the Labrador Sea, where the mesoscale eddies play important roles, to study mesoscale eddies' roles in these areas.

 
Frontier Newsletter/No.26
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