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Impacts of Global Warming on Hydrological Cycles in the Asian Monsoon Region

Advances in Atmospheric Sciences 2008年第6期25卷 960-973页

作者： koji dairaku Seita EMORI Toru NOZAWA Storm Flood and Landslide Research Department National Research Institute for Earth Science and Disaster Prevention Climate Risk Assessment Research Section Center for Global Environmental Research National Institute for Environmental Studies Atmospheric Physics Section Atmospheric Environment Division National Institute for Environmental Studies

The hydrologic changes and the impact of these changes constitute a fundamental global-warmingrelated concern. Faced with threats to human life and natural ecosystems, such as droughts, floods, and soil erosion, water resource planners must increasingly make future risk assessments. Though hydrological predictions associated with the global climate change are already being performed, mainly through the use of GCMs, coarse spatial resolutions and uncertain physical processes limit the representation of terrestrial water/energy interactions and the variability in such systems as the Asian monsoon. Despite numerous studies, the regional responses of hydrologic changes resulting from climate change remains inconclusive. In this paper, an attempt at dynamical downsealing of future hydrologic projection under global climate change in Asia is addressed. The authors conducted present and future Asian regional climate simulations which were nested in the results of Atmospheric General Circulation Model （AGCM） experiments. The regional climate model could capture the general simulated features of the AGCM. Also, some regional phenomena such as orographic precipitation, which did not appear in the outcome of the AGCM simulation, were successfully produced. Under global warming, the increase of water vapor associated with the warmed air temperature was projected. It was projected to bring more abundant water vapor to the southern portions of India and the Bay of Bengal, and to enhance precipitation especially over the mountainous regions, the western part of India and the southern edge of the Tibetan Plateau. As a result of the changes in the synoptic flow patterns and precipitation under global warming, the increases of annual mean precipitation and surface runoff were projected in many regions of Asia. However, both the positive and negative changes of seasonal surface runoff were projected in some regions which will increase the flood risk and cause a mismatch between water

关键词： hydrologic change dynamical downscaling regional climate model Asian monsoon region

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Vacuum Insulation and Achievement of 980 keV,185 A/m^2 H-Ion Beam Acceleration at JAEA for the ITER Neutral Beam Injector

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Plasma Science and Technology 2013年第2期15卷 179-183页

作者： Hiroyuki TOBARI Masaki TANIGUCHI Mieko KASHIWAGI Masayuki dairaku Naotaka UMEDA Haruhiko YAMANAKA Kazuki TSUCHIDA Jumpei TAKEMOTO Kazuhiro WATANABE Takashi INOUE Keishi SAKAMOTO Japan Atomic Energy Agency (JAEA) Mukouyama 801-1 Naka Ibaraki 311-1093 Japan

Abstract Vacuum insulation of -1 MV is a common issue for the HV bushing and the accel- erator for the ITER neutral beam injector （NBI）. The HV bushing as an insulating feedthrough has a five-stage structure and each stage consists of double-layered insulators. To sustain -1 MV in vacuum, reduction of electric field at several triple points existing around the double-layered insulators is a critical issue. To reduce electric field simultaneously at these points, three types of stress ring have been developed. In a voltage holding test of a full-scale mockup equipped with these stress rings, 120% of rated voltage was sustained and the voltage holding capability required in ITER was verified. In the MeV accelerator, whose target is the acceleration of a H- ion beam of 1 MeV, 200 A/mS, the gap between the grid support was extended to suppress breakdowns triggered by electric field concentration at the edge and corner of the grid support. This modi- fication improved the voltage holding capability in vacuum, and the MeV accelerator succeeded in sustaining -1 MV stably, b-~rthermore, it appeared that the H- ions beam was deflected and a part of the beam was intercepted at the acceleration grid, This causes high heat load on the grids and breakdowns during beam acceleration. To suppress the direct interception, a new grid was designed with proper aperture displacement based on a three dimensional beam trajectory analysis, As a result, 980 keV, 185 A/ms H- ion beam acceleration has been demonstrated, which is close to the ITER requirement.

关键词： neutral beam injector (NBI) negative ion beam HV bushing vacuum insu-lation

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γ-ray Spectroscopy of Hypernuclei:Recent KEK Results and Future Plans at J-PARC

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原子核物理评论 2009年第S1期26卷 34-38页

作者： S.Ajimura K.Aoki M.dairaku H.Fujioka T.Fukuda K.Futatsugawa K.Hosomi W.Imoto M.Kawai Y.Kakiguchi S.Kinoshita T.Koike N.Maruyama M.Mimori S.Minami Y.Miura K.Miwa Y.Miyagi T.Nagae D.Nakajima H.Noumi K.S hirotori T.Suzuki T.Takahashi T.N.Takahashi K.Tanida N.Terada A.Toyoda K.Tsukada M.Ukai H.Tamura Department of Physics Osaka University High Energy Accelerator Research Organization (KEK) Department of Physics Kyoto University Department of Physics University of Tokyo Osaka Electro-Communication University Department of Physics Tohoku University RIKEN

In this proceeding,we will first outline the experimental setup and main results of the most recent hypernuclear γ-ray spectroscopy experiment (KEK-E566) performed at KEK-PS K6 beam line. The main feature and characteristics of this type of research will be emphasised. After that,the approved experimental proposal (E13) at J-PARC facility will be introduced briefly.

关键词： γ-ray spectroscopy hypernuclei

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Measurement of Gamma-Rays from ^11 A B and ^12 A C

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Chinese Physics Letters 2007年第8期24卷 2216-2218页

作者：傅元勇周书华 T. Koike S. Kinoshita Y. Ma Y. Miura K. Miwa Y. Miyagi K. Shirotori T. Suzuki H. Tamura K. Tsukada M. Ukai K. Futatsukawa K. Hosomi M. Kawai M. Mimori N. Terada N. Maruyama K. Aoki H Fujioka Y Kakiguchi T. Nagae D. Nakajima H Noumi T Takahashi T.N. Takahashi A. Toyota M. dairaku T. Fukuda S. Minami W. Imoto S. Aiimura K. Tanida China Institute of Atomic Energy PO Box 275(18) Beijing 102413 Department of Physics Tohoku University Sendal 980-8578 Japan High Energy Accelerator Research Organization (KEK) Tsukuba Ibaraki 305-0801 Japan Department of Physics Kyoto University Kyoto 606-8502 Japan Osaka Electro-Communication University Osaka 572-8530 Japan Department of Physics Osaka University Osaka 560-0043 Japan RIKEN Wako 351-0198 Japan

From the ^12 C（π^＋,K^＋）^12 AC reaction the γ -rays of 261.6±0.24 ke V（7/2^＋ →5/2^＋）and 1481.7±0.7 ke V（1/2^＋ →5/2^＋） of ^11 A B,and 2667.3±2.8 keV（1^- 2 → 2^- 1）of ^12 A C hypernuclei have been identified using a large germanium detector array Hyperball2 at K6 beam line of KEK. The observed energies of the transitions 1481.7keV and 261.6 keV are significantly different from the values predicted by the shell model using the △ and SN parameters determined from the ^7 △ Li data.

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