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詳細

森本　昭彦 (モリモト　アキヒコ)

  • 沿岸環境科学研究センター　教授
Last Updated :2020/09/16

研究者情報

学位

  • 博士（理学）（九州大学）

ホームページURL

J-Global ID

研究分野

  • 自然科学一般 / 大気水圏科学

経歴

  • 2015年04月 - 現在  愛媛大学沿岸環境科学研究センター教授
  • 2007年04月 - 2015年03月  名古屋大学地球水循環研究センター・准教授Hydrospheric Atmospheric Research Center
  • 2003年10月 - 2007年03月  名古屋大学地球水循環研究センター・助教授Hydrospheric Atmospheric Research Center
  • 2001年03月 - 2003年09月  独立行政法人水産大学校・助手
  • 1997年04月 - 2001年02月  愛媛大学工学部・教務職員Faculty of Engineering
  • 名古屋大学

学歴

  • 1990年04月 - 1994年03月   愛媛大学   工学部   海洋工学科

所属学協会

  • 日本海洋学会沿岸海洋研究会   

研究活動情報

論文

  • Complementary Remote Sensing Observations of the Tsushima Warm Current Patterns. Remote Sensing of the Asian Seas
    Ichikawa, K, Yoshikawa, Y, Morimoto, A, Fukudome, K, Yoon, J-H
    Barale V. and M. Gade (eds), Springer 191 - 204 2019年 [査読有り]
     研究論文（学術雑誌）
  • Response of lower trophic ecosystem in the Japan Sea to horizontal nutrient flux change through the Tsushima Strait
    Shibano, R, Morimoto, A, Takayama, K, Takikawa, T, Ito, M
    Estuarine, Coastal and Shelf Science 229 106386 2019年 [査読有り]
     研究論文（学術雑誌）
  • Future Prediction of nutrient concentration and primary production in the Japan Sea
    Morimoto, A, Shibano, R. Ito, M, Takikawa, T
    Integrated Coastal Management in the Japanese Satoumi, Elsevier 94 - 102 2019年 研究論文（その他学術会議資料等）
  • Xiaojie Yu, Xinyu Guo, Akihiko Morimoto, Anukul Buranapratheprat
    Continental Shelf Research 153 16 - 29 2018年02月 [査読有り]
     研究論文（学術雑誌） 
    River plumes are a general phenomenon in coastal regions. Most previous studies focus on river plumes in middle and high latitudes with few studies examining those in low latitude regions. Here, we apply a numerical model to the Upper Gulf of Thailand (UGoT) to examine a river plume in low latitudes. Consistent with observational data, the modeled plume has seasonal variation dependent on monsoon conditions. During southwesterly monsoons, the plume extends northeastward to the head of the gulf during northeasterly monsoons, it extends southwestward to the mouth of the gulf. To examine the effects of latitude, wind and river discharge on the river plume, we designed several numerical experiments. Using a middle latitude for the UGoT, the bulge close to the river mouth becomes smaller, the downstream current flows closer to the coast, and the salinity in the northern UGoT becomes lower. The reduction in the size of the bulge is consistent with the relationship between the offshore distance of a bulge and the Coriolis parameter. Momentum balance of the coastal current is maintained by advection, the Coriolis force, pressure gradient and internal stresses in both low and middle latitudes, with the Coriolis force and pressure gradient enlarged in the middle latitude. The larger pressure gradient in the middle latitude is induced by more offshore freshwater flowing with the coastal current, which induces lower salinity. The influence of wind on the river plume not only has the advection effects of changing the surface current direction and increasing the surface current speed, but also decreases the current speed due to enhanced vertical mixing. Changes in river discharge influence stratification in the UGoT but have little effect on the behavior of the river plume.
  • Taketoshi Kodama, Akihiko Morimoto, Tetsutaro Takikawa, Masashi Ito, Yosuke Igeta, Shoko Abe, Ken-ichi Fukudome, Naoto Honda, Osamu Katoh
    JOURNAL OF OCEANOGRAPHY 73 6 759 - 769 2017年12月 [査読有り]
     研究論文（学術雑誌） 
    To identify water with an excess nitrate concentration to phosphate ratio and its potential source, the nutrient concentrations in the Tsushima Strait (TSS) were investigated over ten cruises in August and September 2007-2014, excluding 2010. On the basis of the Redfield ratio, water with an excess nitrate concentration of > 1 mu M (positive ExNOx water) was identified below the surface mixed layer during four cruises in 2011-2013. Positive ExNOx water was present mainly in less-saline (< 34) waters with a density of 22-25 sigma (theta) , and 25-75 m depth. However, in August 2012, positive ExNOx was detected in dense (25-25.5 sigma(theta) ) and deep (50-110 m depth) waters near the salinity maximum, although the salinity during this period was significantly lower than that in other years. The horizontal length of positive ExNOx water was > 100 km across the TSS during two cruises in August 2012 and September 2013, respectively. According to multi-regression analysis conducted on the silicate concentration, temperature, and salinity, the silicate concentration was increased in the less-saline subsurface water. The required amount of original freshwater was 10(8-9) m(3) day(-1) based on the excess nitrate concentration. This evidence indicates that the positive ExNOx water originated from large river waters such as the Changjiang. Thus, discharged water from the rivers of the East Asia is contributing to the increased N:P ratio in the Tsushima Warm Current, southern Japan Sea.
  • M. Inoue, Y. Shirotani, Y. Furusawa, K. Fujimoto, H. Kofuji, K. Yoshida, S. Nagao, M. Yamamoto, Y. Hamajima, N. Honda, A. Morimoto, T. Takikawa, A. Shiomoto, Y. Isoda, M. Minakawa
    CONTINENTAL SHELF RESEARCH 143 167 - 174 2017年07月 [査読有り]
     研究論文（学術雑誌） 
    We investigated lateral profiles of Ra-228 (half-life; 5.75 years) activity and Ra-228/Ra-226 (1600 years) activity ratio using 241 surface water samples collected in/around the Sea of Japan and the East China Sea (ECS) during June October of 2009-2014. In the ECS, the Ra-228/Ra-226 ratio in the surface waters exhibited markedly wide variation ( < 0.05-3.5) in June, predominantly reflecting the mixing between the Ra-228-rich continental shelf water and the Ra-228-depleted Kuroshio Current water. In July, the surface waters of the central Sea of Japan (135-138 degrees E) became separated into three currents: the Offshore Branch of the Tsushima Warm Current (OBTWC) (Ra-228/Ra-226 =0.7-1.2) at 39-41 degrees N, the Coastal Branch of the TWC (CBTWC) (similar to 0.7) on the southern side, and sub-Arctic Current (similar to 0.7) on the northern side. From the central to northeastern Sea of Japan, the Ra-228/Ra-226 ratio at the surface (0.8-1.0) was within a range between that of the CBTWC and OBTWC. The fraction of continental shelf water in the CBTWC, OBTWC, and in their combined current was estimated to be 11-16%, similar to 8%, and 10-11%, respectively.
  • Tetsutaro Takikawa, Toshiteru Watanabe, Tomoharu Senjyu, Akihiko Morimoto
    CONTINENTAL SHELF RESEARCH 143 271 - 277 2017年07月 [査読有り]
     研究論文（学術雑誌） 
    This study found an unusually large variation in the coastal sea level difference (SLD) in the southwestern Japan Sea from July to October 2013. The time and horizontal scales were about 4 months and 1000 km along the coast, respectively. During the exceptionally hot summer of 2013, strong monsoon winds blew through the Tsushima Straits into the southwestern Japan Sea, because the North Pacific High was located farther west than average. The southwesterly winds averaged 7 m s(-1) parallel to the coast in July 2013, resulting in Ekman transport toward the coast. The most noticeable SLD was measured between Omijima and Mishima, normal to the 250 km rectilinear coastal line. The velocity of the first branch of the Tsushima Warm Current increased to about 50 cm s(-1) between Omijima and Mishima from late July to early August. Although the SLD seemed to simultaneously increase and decrease along the Japanese coast with large time scale, the variation in coastal SLD propagated along the Japanese coast, reaching Niigata-nishi in the eastern Japan Sea. The propagation speed in the wide continental shelf of the southern Japan Sea was much higher than that in the narrow eastern shelf, which was consistent with the behavior of continental shelf waves.
  • Tetsutaro Takikawa, Akihiko Morimoto, Goh Onitsuka
    JOURNAL OF OCEANOGRAPHY 72 4 529 - 540 2016年08月 [査読有り]
     研究論文（学術雑誌） 
    From summer to autumn, in the southwestern Japan Sea, the maximum subsurface nutrient (DIN: nitrate + nitrite) concentration and minimum dissolved oxygen (DO) concentration layers lie at depths of approximately 75-125 dbar. The subsurface nutrient-rich water originates from the East China Sea through the lower layer (50-100-dbar depths) of the Tsushima Straits. On a smaller scale, in the subsurface nutrient-rich layer, submesoscale structures (similar to 10 km) with high DO and chlorophyll-a (Chl-a) concentrations were observed below the surface euphotic zone and the minimum Chl-a layer in late October 2008. Considering that photosynthesis cannot occur in the minimum Chl-a layer, the submesoscale Chl-a maxima did not coincide with the normal maximum subsurface chlorophyll layer, where phytoplankton can mature, in the seasonal pycnocline in summer. The subsurface submesoscale water masses were zonally distributed from west to east downstream of the Tsushima Warm Current. In late November 2008, high DO and Chl-a water subducted from the surface density front to the subsurface layers along the isopycnal surface. In the large-scale frontal region of the Tsushima Warm Current, the subsurface isopycnals were convex upward both in October and November 2008, suggesting meso- and submesoscale upwellings.
  • Anukul Buranapratheprat, Pontipa Luadnakrob, Tetsuo Yanagi, Akihiko Morimoto, Fangli Qiao
    CONTINENTAL SHELF RESEARCH 118 100 - 110 2016年04月 [査読有り]
     研究論文（学術雑誌） 
    Water column conditions in the Gulf of Thailand (GoT) were analyzed by considering four major factors including surface heat fluxes, freshwater inputs from river discharge and atmospheric fluxes, tidal and wind stirrings. The analytical results suggested that surface heat fluxes and tidal stirring are the most important factors to control water column conditions, followed by freshwater fluxes. Well-mixing was predicted to occur from November to February resulted from relatively large tidal stirring, surface heat loss and low freshwater input, but the climatological density data suggested stratification during this period because of local freshwater accumulation. The South China Sea (SCS) and the northeast wind played significant contributions to freshwater accumulation by generating surface water flow into the gulf during the northeast monsoon. On the other hand, the development of stable and strong stratification during the southwest monsoon was enhanced by SCS subsurface water intrusion and surface outflow induced by the southwest wind. Strong surface heat fluxes coincident with SCS intrusion in April and May make water stratification more complex. This phenomenon generates double thermocline and multi-stratified water in some GoT area. (C) 2016 Elsevier Ltd. All rights reserved.
  • 日本によるアジアにおける海洋研究－WESTPAC創立25年の活動を中心に－
    安藤健太郎, 岩滝光儀, 植松光夫, 大野浩史, 北沢一宏, 小松輝久, 鈴木敏之, 勢田明大, 西田周平, 福代康夫, 松野健, 道田豊, 森本 昭彦
    海の研究 24 3 79 - 108 2015年 [査読有り]
     研究論文（学術雑誌）
  • Masashi Ito, Akihiko Morimoto, Tatsuro Watanabe, Osamu Katoh, Tetsutaro Takikawa
    PROGRESS IN OCEANOGRAPHY 121 83 - 93 2014年02月 [査読有り]
     研究論文（学術雑誌） 
    We compiled a long-term record of monthly mean sea surface currents in the Japan Sea from satellite altimetry and satellite-tracked drifter data. The record covers the entire Japan Sea for the period from May 1995 through January 2009. Using these data, we examined the path of the Tsushima Warm Current in the southwestern part of the Japan Sea. The mean sea surface current field revealed a "triple-branch" pattern. The first branch through the eastern channel of the Tsushima Strait flows along the coast ofJapan with a mean current velocity of 20 cm s(-1). The second branch flows along the continental shelf edge at around the 200-m isobath with a mean current velocity of 12 cm s(-1). The third branch flows along the east coast of the Korean peninsula with a mean current velocity of 25 cm s(-1). We investigated seasonal variation in the path of each branch. The first branch flowing along the Japanese coast throughout the year is highly stable. The second branch is stable throughout the year except in November. The third branch flowing along the east coast of Korea is highly stable until 38 degrees N. Downstream of the third branch around 38 degrees N, the current bifurcates into northeastward and southeastward currents. The northeastward current exhibits stable flow from June to February except in January. This current joins an eastward current originating around 39 degrees N, 128.5 degrees E. The southeastward current flows stably in June, September, and December. There were two current paths east of 131 degrees E over the continental shelf off the San'in coast of Japan. The nearshore current flows along the Japanese coast with a mean current velocity of 23 cm s(-1), and the offshore current flows around the continental shelf area with a mean current velocity of 19 cm s(-1). These two currents are highly stable throughout the year. A current flows to the west of Oki Island to around 38.5 degrees N and is highly stable in all months except March to July. These results provide a schematic view of the paths of the Tsushima Warm Current in the southwestern part of the Japan Sea. (c) 2013 Elsevier Ltd. All rights reserved.
  • 大気海洋波浪結合モデルの開発と台風実験への応用
    相木秀則, 吉岡真由美, 加藤雅也, 森本昭彦, 篠田太郎, 坪木和久
    沿岸海洋研究 52 2 139 - 148 2014年02月 [査読有り]
     研究論文（学術雑誌）
  • 対馬海峡を通過する溶存無機窒素の水平輸送量
    森本昭彦, 後藤暁, 滝川哲太郎, 千手智晴, 伊藤雅, 鬼塚剛, 渡邉敦, 杢雅利
    海と空 89 2 27 - 35 2013年12月 [査読有り]
     研究論文（学術雑誌）
  • 宗谷、津軽、対馬海峡周辺における海面高度偏差と対馬暖流の季節変動
    滝川哲太郎, 伊藤雅, 福留研一, 森本昭彦, 広瀬直毅, 尹宗煥
    海と空 89 2 37 - 44 2013年12月 [査読有り]
     研究論文（学術雑誌）
  • T. Komatsu, S. Mizuno, A. Natheer, A. Kantachumpoo, K. Tanaka, A. Morimoto, S-T. Hsiao, E. A. Rothausler, H. Shishidou, M. Aoki, T. Ajisaka
    J. Appl. Phycol 2013年11月 [査読有り]
     研究論文（学術雑誌）
  • Daisuke Takahashi, Akihiko Morimoto
    PROGRESS IN OCEANOGRAPHY 111 125 - 139 2013年04月 [査読有り]
     研究論文（学術雑誌） 
    An analysis of a surface flow field in the East China Sea (ECS) obtained by combining satellite altimeter and drifter data provides comprehensive information of its mean field and annual variation. The Taiwan Warm Current, the onshore Kuroshio intrusion, the Kuroshio, the northeastward Kuroshio branch, the northward current west of Kyushu, the Cheju Warm Current, and the Tsushima Warm Current are regarded as persistent currents. Annual variation is a dominant signal in the ECS and is a major component of the seasonal variation. The contribution of the annual variation to the seasonal variation is estimated as 50% over the ECS, and exceeds 70% for the Kuroshio northeast of Taiwan, the Taiwan Warm Current, the Taiwan Strait Warm Current, the onshore Kuroshio intrusion, the northeastward Kuroshio branch, the northward current west of Kyushu, and the Tsushima Warm Current. The annual variation is characterized by propagation of vorticity anomalies from northeast of the Taiwan Strait and in the Tsushima Strait. The vorticity anomaly from northeast of the Taiwan Strait propagates downstream in the northeastward Kuroshio branch along isobaths of about 100 m on the shelf edge. In contrast, the vorticity anomaly in the Tsushima Strait propagates upstream of the Tsushima Warm Current along isobaths of 100-200 m. The propagation of the vorticity anomalies causes the annual variation with a phase difference in the northeastward Kuroshio branch and the northward current west of Kyushu, and the behavior of the vorticity anomalies can be well explained as a first approximation by a dispersion relation of a quasigeostrophic topographic Rossby wave propagating in a mean flow. Generation of the vorticity anomalies from northeast of the Taiwan Strait and in the Tsushima Strait appears to be closely related to the annual variation of the Kuroshio's current speed northeast of Taiwan and of volume transport through the Tsushima Strait, respectively. (C) 2013 Elsevier Ltd. All rights reserved.
  • Ichikawa, K, Morimoto, A, Yoshikawa, Y, Liu, C.-T, Sugitani, S, Lai, J.-W, Yang, W. C, Liang, E. Y, Yufu, K, Kyushima, M, Fujii, S, Senju, T, Ide, Y
    Ocean Science Journal 48 1 141 - 148 2013年01月 [査読有り]
     研究論文（学術雑誌）
  • Akihiko Morimoto, Atsushi Watanabe, Goh Onitsuka, Tetsutaro Takikawa, Masatoshi Moku, Tetsuo Yanagi
    PROGRESS IN OCEANOGRAPHY 105 38 - 46 2012年10月 [査読有り]
     研究論文（学術雑誌） 
    We conducted hydrographic observations 23 times across the eastern channel of the Tsushima/Korea Straits (ECTKS) to estimate material transports from 2005 to 2008. Freshwater and nutrient transports through the ECTKS became high from summer to autumn, with quite large interannual variations. Freshwater and dissolved inorganic nitrogen (DIN) transport in 2007 was much lower than in other years. The interannual variation in freshwater transport seemed to show almost the same pattern as that of the volume transport of the Tsushima Warm Current and Changjiang discharge. However, we could not explain the interannual variation in freshwater transport quantitatively. The DIN transport in August 2007 was approximately one third of that in 2005 due to the much lower DIN concentration in the bottom layer of the ECTKS in 2007 than in 2005. The difference of DIN concentration between the years was caused by different water mass intrusions into the ECTKS. Water mass analysis and alkalinity data revealed that the water mass in 2005 came from the Yellow Sea or the shelf of the East China Sea, while that in 2007 came from the Kuroshio region. Examination of long-term water temperature data indicated that the origin of ECTKS water masses has changed many times in the past. We suggest that variations of the Changjiang discharge and wind field over the Yellow and East China seas might relate to the change of water mass in the ECTKS. (c) 2012 Elsevier Ltd. All rights reserved.
  • Daisuke Takahashi, Akihiko Morimoto, Tetsuya Nakamura, Takuji Hosaka, Yoshihisa Mino, Vu Hai Dang, Toshiro Saino
    PROGRESS IN OCEANOGRAPHY 105 47 - 60 2012年10月 [査読有り]
     研究論文（学術雑誌） 
    Short-term flow and water temperature fluctuations in Sagami Bay were examined using mooring and hydrographic data observed during the non-large-meander path (NLM) of the Kuroshio. In the surface layer (<150 m), the flow fluctuation is predominant and is excited by the sudden strong eastward flow with speeds greater than 20 cm s(-1) in the central part of the bay. This flow is a part of an intrusion of Kuroshio water via the Oshima West Channel into the bay and/or a cyclonic circulation in the northern part of the bay. The cyclonic circulation, which is approximately balanced under the geostrophic flow relationship, is mainly generated or enhanced by the intrusion, which is accompanied by eastward propagation of the small meander of the Kuroshio south of Japan during the transition from the nearshore non-large-meander path (nNLM) to the offshore non-large-meander path (oNLM), regardless of season. The water temperature fluctuation in the subsurface layer (similar to 150 m) is caused by upwelling of cold deeper water and is closely related to the eastward flow fluctuations in the surface layer in the central part of the bay. Our analysis leads us the conclusion that the upwelling occurs as the response of the subsurface density field to the surface flow field under the Earth's rotation. Additionally, the intrusion of Kuroshio water via the Oshima West Channel tends to cause, not only cyclonic circulation and upwelling in the northern part of the bay, but also the Kyucho, which is the coastal density current under the Earth's rotation, in the bay's coastal area during the non-large-meander path (NLM). (C) 2012 Elsevier Ltd. All rights reserved.
  • Tetsutaro Takikawa, Goh Onitsuka, Ken-ichi Fukudome, Jong-Hwan Yoon, Akihiko Morimoto
    PROGRESS IN OCEANOGRAPHY 105 30 - 37 2012年10月 [査読有り]
     研究論文（学術雑誌） 
    The seasonal variation of counterclockwise eddies downstream of the Tsushima Islands in the Tsushima Straits was investigated from 2004 to 2008 using long-term acoustic Doppler current profiler (ADCP) data. Eddy activity was high from summer to autumn (July-November). The eddies were formed in short-term intervals of 5-8 days, almost corresponding to the formation cycle of Karman vortices. The eddy activity varied on a longer time period (about 13 days). The mean kinetic energy (MKE) converted to eddy kinetic energy (EKE) at current shears between the eastern and western channels of the Tsushima Straits. The counterclockwise eddies that formed downstream of the Tsushima Islands were intensified and maintained by energy conversion from MKE to EKE at the northern shear of the current core in the eastern channel. The countercurrent east of the Tsushima Islands from summer to autumn was intensified by energy conversion from EKE to MKE. (c) 2012 Elsevier Ltd. All rights reserved.
  • Jae-Hong Moon, Naoki Hirose, Akihiko Morimoto
    JOURNAL OF OCEANOGRAPHY 68 2 345 - 354 2012年04月 [査読有り]
     研究論文（学術雑誌） 
    A simple effective method of inverse estimation provided by model Green's functions is examined to calibrate tides in a regional circulation model for the East Asian marginal seas. The Green's function optimization derived by perturbing the model parameters significantly improves the estimate relative to observation as compared with baseline integration. Among the optimized model parameters, the largest effects on cost function reduction come first from the harmonic constant of M-2 along the open boundaries with the optimized values of 89.7 +/- A 0.8% for amplitude, and second from the bottom friction with the optimized value of (3.06 +/- A 0.08) x 10(-3).
  • Tetsutaro Takikawa, Goh Onitsuka, Ken-ichi Fukudome, Jong-Hwan Yoon, Akihiko Morimoto, Masatoshi Moku, Atsushi Watanabe
    ESTUARIES AND COASTS 34 4 775 - 784 2011年07月 [査読有り]
     研究論文（学術雑誌） 
    Horizontal, vertical and temporal distribution of a cyclonic (counterclockwise) eddy, where biological productivity is high, downstream of the Tsushima Islands in the eastern channel of the Tsushima Straits in November 2007 was revealed using conductivity-temperature-depth and acoustic Doppler current profiler data. The eddy had a horizontal scale of approximately 40-60 km, and the accompanying baroclinic current was more than 15 cm s(-1) at the edge of the eddy. The island-induced cyclonic eddy moved east-northeastward at about 10 km day(-1) (similar to 10 cm s(-1)) along the Tsushima Warm Current and was intensified by the barotropic instability in the current shear. The cyclonic eddy with high surface chlorophyll a concentrations intensified in the vicinity of the Tsushima Islands and was advected by the Tsushima Warm Current towards the southwestern Japan Sea.
  • 黒潮の非大蛇行離岸流路期における相模湾の50-70日周期の流速変動
    高橋大介, 森本昭彦, 中村哲也, 保坂拓志, 三野義尚, 才野敏郎
    海の研究 20 3,4 55 - 79 2011年 [査読有り]
     研究論文（学術雑誌）
  • 2007年11月に対馬東部海域で観測された低気圧性渦周辺の栄養塩・プランクトン分布
    鬼塚剛, 滝川哲太郎, 小針統, 杢雅利, 森本昭彦, 渡邉敦, 吉川裕, 柳哲雄
    海と空 87 1 11 - 19 2011年 [査読有り]
     研究論文（学術雑誌）
  • 2009年初夏，隠岐諸島東方海域における海洋構造と大型クラゲ(Nemopilema nomurai)分布
    滝川哲太郎, 秦一浩, 上野俊士郎, 河村真理子, 森本昭彦, 宮地邦明
    海と空 86 1 13 - 22 2010年11月 [査読有り]
     研究論文（学術雑誌）
  • 対馬海峡を通過する栄養塩輸送量の季節・経年変化
    森本昭彦, 滝川哲太郎, 鬼塚剛, 渡邉敦, 杢雅利, 柳哲雄
    月刊海洋 42 10 554 - 560 2010年
  • Development of algorithms for estimating the seasonal nitrate profiles in the upper water column of the Sagami Bay, Japan
    A. A. Hutahaean, J. Ishizaka, A. Morimoto, J. Kanda, N. Horimoto, T. Saino
    La Mer 48 1 - 16 2010年 [査読有り]
     研究論文（学術雑誌）
  • Interannual variations in material transport through the eastern channel of the Tsushima/Korea Straits
    A. Morimoto, A. Watanabe, G. Onitsuka, T. Takikawa, M. Moku, T. Yanagi
    Progress in Oceanography accepted 2010年 [査読有り]
     研究論文（学術雑誌）
  • Daisuke Takahashi, Xinyu Guo, Akihiko Morimoto, Shoichiro Kojima
    CONTINENTAL SHELF RESEARCH 29 15 1896 - 1907 2009年08月 [査読有り]
     研究論文（学術雑誌） 
    An analysis of surface current data obtained from 2002 to 2005 using long-range high-frequency radar provides the first evidence for the presence of biweekly (11-14 day) periodic variations of the Kuroshio axis northeast of Taiwan. This analysis clarifies the spatio temporal characteristics of these variations and reveals that cyclonic/anticyclonic eddies propagating along the shelf slope from the vicinity of the deep channel east of Taiwan induce these variations northeast of Taiwan. The behavior of the cyclonic/anticyclonic eddies on the shelf slope is well explained by 2nd-mode interior shelf waves advected by the Kuroshio's mean flow. Remote effects from the vicinity of the deep channel east of Taiwan, or from outside the East China Sea, are believed to play an important role in the generation of these biweekly periodic variations of the Kuroshio axis northeast of Taiwan. Moreover, on the shelf slope, these variations cause an on shore current across the shelf slope, suggesting topographically controlled upwelling. Therefore, the biweekly periodic variations of the Kuroshio axis northeast of Taiwan might contribute not only to the on shore transport of Kuroshio surface water but also to transport nutrient-rich Kuroshio subsurface water on to the shelf in the East China Sea. (C) 2009 Elsevier Ltd. All rights reserved.
  • Akihiko Morimoto, Yutaka Isoda, Tatsuji Tameishi, Shimpei Moriwaki
    CONTINENTAL SHELF RESEARCH 29 11-12 1437 - 1447 2009年06月 [査読有り]
     研究論文（学術雑誌） 
    Using long-term sea surface temperature (SST) and acoustic Doppler current profiler (ADCP) data, we examined variations in the current axis of the Tsushima Warm Current (TWC) off the San'in coast of Japan, near the entrance to the Japan Sea. There were large horizontal temperature gradients along the shelf edge in the southwestern Japan Sea from October to May, suggesting that the second branch of the TWC appears not only in spring and autumn but also in winter. From the ADCP data analysis, we found that currents with speeds of approximately 20 cm s(-1) and greater appeared around the shelf edge off San'in coast in all seasons. The SST and ADCP data analyses suggested that the second branch of the TWC exists around the shelf edge off the San'in coast throughout the year. This finding differed from those of previous studies. A relatively strong current (speed greater than 15 cm s(-1)) appeared on the shore side in all seasons, except at line W in winter. This current might be the first branch of the TWC. The first branch seemed to occur around in 100 m isobaths, but shifted northward and southward because the bottom topography around lines W and M was relatively flat and the shelf was broad. The first branch was very obscure, and it was difficult to define the two branches of the TWC off the San'in coast from the seasonally averaged vectors. However, snapshots of current distribution derived from the ADCP data clearly showed these branches. Hence, both the first and second branches might occur throughout the year off the San'in coast. (C) 2009 Elsevier Ltd. All rights reserved.
  • Eko Siswanto, Akihiko Morimoto, Shoichiro Kojima
    GEOPHYSICAL RESEARCH LETTERS 36 L11603  2009年06月 [査読有り]
     研究論文（学術雑誌） 
    The enhancement of primary productivity (PPenh) in the southern East China Sea (ECS) following 16 typhoon passages was investigated using ocean color data and a primary productivity model. PPenh tended to be higher when typhoons traversed slowly with trajectories that allowed strong southerly winds to prevail over Yonaguni Island. Such long-lasting southerly winds were believed to push the Kuroshio current axis shelfward, enhancing the upwelling of nutrients, hence promoting new productivity (NP). The importance of long-lasting southerly winds as a proxy for physical perturbations underlying PPenh was expressed by an empirical equation by which 88% of PPenh variation could be explained. Applying this equation, we assessed that typhoon passages accounted for a minimum of 0.6-11.8% of the ECS summer-fall NP, suggesting that typhoon passage over the southern ECS is an important phenomenon supporting NP in the ECS. Citation: Siswanto, E., A. Morimoto, and S. Kojima (2009), Enhancement of phytoplankton primary productivity in the southern East China Sea following episodic typhoon passage, Geophys. Res. Lett., 36, L11603, doi: 10.1029/2009GL037883.
  • Akihiko Morimoto, Shoichiro Kojima, Sen Jan, Daisuke Takahashi
    ESTUARINE COASTAL AND SHELF SCIENCE 82 3 547 - 552 2009年04月 [査読有り]
     研究論文（学術雑誌） 
    We investigated the movement of the Kuroshio axis on the northeast shelf of Taiwan associated with the passage of typhoons, using sea surface current data observed by the ocean radar system on Yonaguni and Ishigaki islands. First, we examined daily Kuroshio axis variation on the northeast shelf of Taiwan during typhoon events. The ocean radar data showed that the Kuroshio axis moved onto the shelf after passages of typhoons. The Kuroshio moved onto the shelf and stayed there after the passage of Typhoon Hai-Tang; while the Kuroshio maintained this pattern, southerly wind blew continuously for 4 days. The mean current speed northeast of Taiwan after the typhoon's passage increased by 18 cm s(-1). In addition, the sea level difference between two satellite altimetry tracks east of Taiwan increased by 14.4 cm. These results suggest that coastal upwelling east of Taiwan caused by the southerly wind generated an east-west sea level difference that, in turn, generated a northward geostrophic current. This current could have enhanced the Kuroshio east of Taiwan, and pushed it onto the shelf. (C) 2009 Elsevier Ltd. All rights reserved.
  • Akihiko Morimoto, Tetsutaro Takikawa, Goh Onitsuka, Atsushi Watanabe, Masatoshi Moku, Tetsuo Yanagi
    JOURNAL OF OCEANOGRAPHY 65 1 61 - 71 2009年02月 [査読有り]
     研究論文（学術雑誌） 
    We conducted hydrographic observations ten times in the Tsushima Strait to reveal seasonal variations of horizontal material transports such as of heat, freshwater, chlorophyll a, and dissolved inorganic nitrogen (DIN) and phosphorus (DIP) through the eastern channel of the Tsushima Strait (ECTS). The volume, freshwater, and heat transport results are of nearly the same order as results reported in previous studies. The annual mean DIN and DIP transports of 3.59 kmol/s and 0.29 kmol/s are large relative to those of the Changjiang and the Taiwan Strait and are horizontally transported through the ECTS. Nutrient transports are high in July-August and October and low in April and November. Increased nutrient transports in July-August and October are due to the appearance of a cold saline water mass in the bottom layer of the ECTS. Changes in DIN transports in summer and autumn, which account for two-thirds of the total annual DIN transport, would have a large effect on the nitrogen budget and biological productivity in the Tsushima Warm Current region.
  • Goh Onitsuka, Akihiko Morimoto, Tetsutaro Takikawa, Atsushi Watanabe, Masatoshi Moku, Yutaka Yoshikawa, Tetsuo Yanagi
    ESTUARINE COASTAL AND SHELF SCIENCE 81 3 401 - 408 2009年02月 [査読有り]
     研究論文（学術雑誌） 
    The relationship between island-induced cyclonic eddies and chlorophyll a (chl-a) was investigated using field data and satellite images in the eastern channel of the Tsushima Straits. The maximum chl-a concentration around the leeward eddy of the Tsushima islands was two or three times greater than that of outside the eddy. Two different mechanisms of chl-a enhancement associated with island-induced cyclonic eddies were found in the post-bloom periods. In summer, when nutrients were depleted in the surface layer, eddy pumping increased the nutrient supply in the euphotic zone, resulting in enhanced chl-a around the shallow thermocline near the eddy core. In late autumn, when the mixed layer deepened over the euphotic zone, the mixed layer depth became shallow due to the doming effect of the cyclonic eddy, therefore, the improved irradiance condition led to an increase in the chl-a concentration in the surface mixed layer. Nighttime satellite visible images showed a number of fishing vessels in the lee region of the Tsushima Islands, implying that the enhanced phytoplankton biomass may have resulted in good feeding conditions for fishes and squids in the Tsushima Straits. (c) 2008 Elsevier Ltd. All rights reserved.
  • Akihiko Morimoto
    Journal of Oceanography 65 4 477 - 485 2009年 [査読有り]
     研究論文（学術雑誌） 
    The magnitude and geographical distribution of the error in the Archiving, Validation and Interpretation of Satellite Oceanographic data (AVISO) altimetry data associated with tidal correction around Asian marginal seas has been revealed. The errors were evaluated by harmonic analysis of the AVISO corrected sea surface heights data (CorSSH). Errors of more than 15 cm of tidal correction were recognized in the western and northern parts of the Yellow Sea, Celebes Sea, Kuril Islands, and the northwestern part of the Okhotsk Sea. It was found that the CorSSH and sea level anomaly (SLA) data downloaded from the AVISO are not available for direct use in those marginal seas. To reduce the tidal correction error, the harmonic constants calculated from the latest tide model and regional tide model were applied as the tidal correction of the Altimetry data. The tidal errors in the Yellow Sea and the northwestern part of the Okhotsk Sea were reduced by approximately 20 cm and 10 cm, respectively. Root mean square differences between the harmonic constants derived from tide models and those derived from altimetry data were calculated. The root mean square differences were large in the Yellow and the Okhotsk Seas. Root sum squares for four principal tidal constituents in the Yellow and East China Seas and Okhotsk Sea were 7.72 cm and 8.36 cm, respectively. © 2009 Springer Science+Business Media B.V.
  • Eko Siswanto, Joji Ishizaka, Akihiko Morimoto, Katsuhisa Tanaka, Kazumaro Okamura, Agus Kristijono, Toshiro Saino
    GEOPHYSICAL RESEARCH LETTERS 35 15 2008年08月 [査読有り]
     研究論文（学術雑誌） 
    We elucidated ocean physical and biogeochemical responses to slow-moving Typhoon Meari using a new method combining Argo float and satellite observations. Meari-driven upwelling brought colder, nutrient-rich deep water to the surface layer, causing sea surface cooling (3-6 degrees C) and threefold enhancement of primary production (PP). Maximum surface cooling (and hence nutrient injection) and peak PP enhancement lagged Meari's passage by 1 and 3 days, respectively, implying that remarkable PP enhancement was attributed to new production (NP). This NP accounted for approximately 3.8% of annual carbon export in the East China Sea (ECS) outer shelf, suggesting that typhoon-driven upwelling is important for biogeochemical processes in the ECS. Given the wide coverage of Argo float and satellite data, our new approach may prompt comparative studies in other basins and advance the understanding of the role of tropical cyclones in the global ocean biogeochemical cycle.
  • Tetsutaro Takikawa, Akihiko Morimoto, Goh Onitsuka, Atsushi Watanabe, Masatoshi Moku
    JOURNAL OF OCEANOGRAPHY 64 4 585 - 594 2008年08月 [査読有り]
     研究論文（学術雑誌） 
    Two different cold waters were found under the surface mixed layer in Tsushima Straits and the southwestern Japan Sea in autumn 2004. One is cold saline water with a low concentration of dissolved oxygen, and the other is cold less saline water with a high concentration of dissolved oxygen. The older saline water originates from the bottom of the East China Sea, strongly influenced by the Kuroshio water with high salinity. The bottom density in the eastern channel of the Tsushima Straits is coincident with that of the East China Sea in autumn, corresponding to the season when the cold saline water was frequently found in the Tsushima Straits. The newer less saline water originates from the front of Tsushima Warm Current between the Tsushima Warm Current water and the surface cold water in the Japan Sea. This water is formed by subduction above the isopycnal surface from the front of the Tsushima Warm Current.
  • 対馬海峡蓋井島周辺海域における長江希釈水と沿岸水の分布
    滝川哲太郎, 鬼塚剛, 秦一浩, 川崎潤二, 下川伸也, 濵口正人, 森本昭彦
    水産大学校研究報告 57 29 - 42 2008年 [査読有り]
     研究論文（学術雑誌）
  • 対馬海峡フェリー航路に沿った航走ADCP観測データからの潮流成分の除去
    滝川哲太郎, 酒井健一, 福留研一, 森本昭彦, 鬼塚 剛, 渡邉 敦, 尹 宗煥, 冨賀見清彦, 鎌野 忠, 秦 一浩
    沿岸海洋研究 45 61 - 68 2007年08月 [査読有り]
  • 2004年初冬季に対馬海峡東水道で観測された低気圧性渦
    鬼塚剛, 滝川哲太郎, 森本昭彦, 三野義尚, 松田龍信, 水谷壮太郎, 今義英, 秦一浩, 小薗宏文, 池田太郎, 酒井健一
    水産大学校研究報告 54 1 25 - 30 2007年03月 [査読有り]
     研究論文（学術雑誌）
  • Distribution of prokaryotic picophytoplankton from Seto Inland Sea to the Kuroshio region, with special reference to 'Kyucho' events
    Toshiya Katano, Atsushi Kaneda, Naoto Kanzaki, Yumiko Obayashi, Akihiko Morimoto, Goh Onitsuka, Hideichi Yasuda, Sotaro Mizutani, Yoshihide Kon, Kazuhiro Hata, Hidetaka Takeoka, Shin-ichi Nakan
    AQUATIC MICROBIAL ECOLOGY 46 2 191 - 201 2007年02月 [査読有り]
     研究論文（学術雑誌） 
    A 'Kyucho' (an intrusion of warm surface water) occurs in the Bungo Channel, located in southwestern Japan. The abundances of Prochlorococcus and Synechococcus during a Kyucho, together with physical and chemical environmental factors, were investigated from the Kuroshio region to the Seto Inland Sea, via Bungo Channel, from 26 November to 5 December 2003. With the occurrence of the Kyucho, oceanic water intruded from the Kuroshio region into the middle of the Bungo Channel. The abundance of Prochlorococcus was the highest in the Kuroshio region and the southern part of the Bungo Channel (> 25 x 10(3) cells ml(-1)), low in the northern part of the Bungo Channel (< 1 x 10(3) cells ml(-1)), and below detection levels in the Seto Inland Sea. A relatively high abundance of Synechococcus cells (> 15 x 10(3) cells ml(-1)) was detected in the Kuroshio region and in the southern part of the Bungo Channel, but the abundance (< 6 x 10(3) cells ml(-1)) was low in other regions. In the Kuroshio region and the southern part of the Bungo Channel, high-phycourobilin (PUB)-type cells were dominant (> 90%); at this location, most of the available light in the deeper layer (> 25 m depth) was in the 450 to 500 nm range, corresponding to the peak absorbance of PUB. In contrast, the abundance of low-PUB-type cells accounted for > 75% of the total in the northern part of the Bungo Channel and in the Seto Inland Sea, where most of the available light in the deeper layer (> 10 m depth) was in the 480 to 560 nm range, including the peak absorbance of both PUB and phycoerythrobilin (PEB). These results indicate that Synechococcus cells of high-PUB type, which have a higher Ex 495:545 (> 1.5; ratio of orange fluorescence intensity excited at 495 nm to that at 545 nm), as well as Prochlorococcus cells were advected to the Bungo Channel by the Kyucho. The co-occurrence of the 2 pigment types of Synechococcus in coastal waters is highly affected by a physical process, such as the Kyucho.
  • A Morimoto, T Matsuda
    IGARSS 2005: IEEE International Geoscience and Remote Sensing Symposium, Vols 1-8, Proceedings 5432 - 5435 2005年 [査読有り]
     研究論文（国際会議プロシーディングス） 
    The altimetry data sets of satellite TOPEX/Poseidon and ERS-2 in the Asian marginal seas, the South China, the East China, the Yellow, the Japan/East and Okhotsk Seas, are produced applying the original tidal correction. In order to obtain a mean sea surface current field in the East China and the Japan/East Seas, the mean sea surface current is evaluated using ARGOS buoy trajectories data and altimetry data. From the mean sea surface current field, it is found that the northward current from the Kuroshio region to the Tsushima/Korea Strait exists throughout the year. The mean current field represents the detailed current feature in the Japan/East Sea such as the current path of Tsushima Warm Current.
  • 吉見湾の潮汐予報
    森本昭彦, 下川伸也
    水産大学校研究報告 50 3 87 - 92 2002年 [査読有り]
     研究論文（学術雑誌）
  • 海面高度計による海表面流動場の推定
    森本昭彦
    沿岸海洋研究 39 27 - 37 2001年 [査読有り]
     研究論文（学術雑誌）
  • A. Morimoto, T. Yanagi
    Journal of Oceanography 57 1 1 - 13 2001年 [査読有り]
     研究論文（学術雑誌） 
    Composite sea surface dynamic heights (CSSDH) are calculated from both sea surface dynamic heights that are derived from altimetric data of ERS-2 and mean sea surface that is calculated by a numerical model. The CSSDH are consistent with sea surface temperature obtained by satellite and observed water temperature. Assuming the geostrophic balance, sea surface current velocities are calculated. It is found that temporal and spatial variations of sea surface circulation are considerably strong. In order to examine the characteristics of temporal and spatial variation of current pattern, EOF analysis is carried out with use of the CSSDH for 3.5 years. The spatial and temporal variations of mode 1 indicate the strength or weakness of sea surface circulation over the entire Japan Sea associated with seasonal variation of volume transport through the Tsushima Strait. The spatial and temporal variations of mode 2 mostly indicate the temporal variation of the second branch of the Tsushima Warm Current and the East Korean Warm Current. It is suggested that this variation is possibly associated with the seasonal variation of volume transport through the west channel of the Tsushima Strait. Variations of mode 3 indicate the interannual variability in the Yamato Basin.
  • Akihiko Morimoto, Koichi Yoshimoto, Tetsuo Yanagi
    Journal of Oceanography 56 3 331 - 344 2000年06月 [査読有り]
     研究論文（学術雑誌） 
    Temporal and spatial variations of sea surface circulation in the South China Sea were revealed with use of altimetric data provided by TOPEX/POSEIDON from December 1992 to October 1997. The estimated distribution of sea surface dynamic heights from altimetric data coincide well with the results of observation by Soong et al. (1995) and Chu et al. (1998). The RMS variability of sea surface dynamic height, which is obtained after tidal correction based on Yanagi et al. (1997), is high in the central part of the South China Sea, the Gulf of Tongking, the Sunda Shelf and the Gulf of Thailand. The high RMS variability in the Gulf of Tongking, the Sunda Shelf and the Gulf of Thailand is due to set up and set down of sea water by the East Asian monsoon, which is northeasterly during winter and southwesterly during summer. Also, the high RMS variability in the central part of the South China Sea is due to the variations of basin-wide circulation. The circulations are dominant in the central part of the South China Sea during summer and winter, an anticyclonic circulation during summer and a cyclonic circulation during winter. It is suggested that these circulations are controlled by the East Asian monsoon. Hence, there is an interannual variability of the basin-wide circulation associated with the variation of the East Asian monsoon.
  • Akihiko Morimoto, Tetsuo Yanagi, Akio Kaneko
    Journal of Oceanography 56 1 31 - 41 2000年02月 [査読有り]
     研究論文（学術雑誌） 
    Satellite altimetric data have been very useful in the study of variation in the eddy field of the ocean. In order to investigate the variation in the eddy field, we have to remove tidal signals from altimetric data. However, global tidal models do not have sufficient accuracy in marginal seas such as the Japan Sea. In this study, we carried out harmonic analysis of temporal fluctuations of sea surface height data in the Japan Sea measured by TOPEX/POSEIDON. We could eliminate the tidal signals from altimetric data of TOPEX/POSEIDON and also from ERS-2 altimetric data with use of the harmonic constants derived from TOPEX/POSEIDON and tide gauge data along the coast. We draw co-tidal and co-range charts in the Japan Sea using the result of the harmonic analysis of TOPEX/POSEIDON altimetric data and tide gauge data along the coast. The results obtained turn out to be very useful for the tidal correction of altimetric data from satellite in the Japan Sea.
  • Akihiko Morimoto, Tetsuo Yanagi, Akio Kaneko
    Journal of Oceanography 56 4 449 - 462 2000年 [査読有り]
     研究論文（学術雑誌） 
    The Japan Sea is one of the eddy-rich areas in the world. Many researchers have described the variability of the eddy field and its structure in the Tsushima Warm Current region. On the other hand, since there are few data covering the northern part of the Japan Sea, we are not able to understand the detailed variability of the eddy field there. The variation of the eddy field in the Japan Sea is investigated using the temporal fluctuations of sea surface height measured by altimetric data from TOPEX/POSEIDON and ERS-2. Tidal signals are eliminated from the altimetric data on the basis of the results of Morimoto et al. (2000). Distributions of sea surface dynamic height are produced by using the optimal interpolation method every month. The distributions warm and cold eddies that we obtained coincide well with the observed isotherms at 100 m depth measured by the Japan Sea National Fisheries Research Institute and the sea surface temperature measured by satellite. There are areas with high RMS variability of temporal fluctuations of sea surface dynamic height in the Yamato Basin, the Ulleung Basin, east of North Korea, the eastern part of the Yamato Rise, the Tsushima Strait and west of Hokkaido. The characteristics of eddy propagation in the high RMS variability regions are examined using a lag correlation analysis. Seasonal variations in the number of warm and cold eddies are also examined.
  • Relationship between the sand waves and the current field in the Bungo Channel, Japan. Interactions between Estuaries, Coastal Seas and Shelf Seas
    Morimoto, A, T. Yanagi
    Ed. by T. Yanagi 217 - 232 2000年 [査読有り]
     研究論文（学術雑誌）
  • 森本昭彦, 柳哲雄
    海の研究 8 119 - 127 1999年 [査読有り]
     研究論文（学術雑誌）
  • Relationship between the sand waves and the current field in the Bungo Channel
    Morimoto, A, Yanagi, T
    Proceedings of 9th PECS Workshop 78 - 79 1998年 [査読有り]
     研究論文（学術雑誌）

講演・口頭発表等

  • 山口県山陰沿岸定線ＡＤＣＰデータによる潮流と平均流の推定  [通常講演]
    都倉雄太, 滝川哲太郎, 森本昭彦, 鎌野忠, 秦一浩
    2018年度九州沖縄地区合同シンポジウム 日本海研究の現状と今後について 2018年12月 口頭発表（一般）
  • 沿岸水位差から推定した山口県見島周辺海域を通過する対馬暖流沿岸分枝の流量変動  [通常講演]
    橋本涼介, 滝川哲太郎, 渡邉俊輝, 千手智晴, 森本昭彦
    2018年度九州沖縄地区合同シンポジウム 日本海研究の現状と今後について 2018年12月 口頭発表（一般）
  • 日本海環境変動予測モデルの構築  [通常講演]
    森本昭彦
    環境省環境研究総合推進費S-13 平成30年度公開成果発表会 2018年11月 口頭発表（一般）
  • 対馬海峡を経由し日本海へ供給される  [通常講演]
    柴野良太, 森本昭彦, 高山勝巳, 滝川哲太郎, 伊藤雅
    日本水産海洋学会 2018年11月 ポスター発表
  • Interannual variability in nutrient transport from the East China Sea to the Japan Sea  [通常講演]
    Morimoto, A, Shibano, R, Takayama, K, Takikawa, T
    The 12th International Conference on the Environmental Management of the Enclosed Coastal Seas 2018年11月 口頭発表（一般）
  • 東シナ海～対馬暖流域における低次生態系モデルの構築  [通常講演]
    柴野良太, 森本昭彦, 高山勝巳, 滝川哲太郎, 伊藤雅
    東京大学大気海洋研究所共同利用研究集会 海洋生態系シンポジウム2018 2018年11月 口頭発表（一般）
  • Long-term changes of COD in the sea area surrounding in Japan  [通常講演]
    Komai, Y, Sugimoto, N, Yabuki, Y, Ono, J, Yamamoto, K, Tanaka, S, Ishikawa, Y, Morimoto, A
    The 12th International Conference on the Environmental Management of the Enclosed Coastal Seas 2018年11月 ポスター発表
  • The Dead zone in Jakarta Bay  [通常講演]
    Hayami, Y, Morimoto, A, Sudaryanto, A, Sachoemar, S, Soeyanto, E, Rusdiansyah, A, Mochamad, S, Sato, S
    The 12th International Conference on the Environmental Management of the Enclosed Coastal Seas 2018年11月 口頭発表（一般）
  • A numerical experiment to investigate the residence time of water mass in the Gulf of Thailand  [通常講演]
    Leenawarat, D, Buranapratheprat, A, Morimoto, A
    The 12th International Conference on the Environmental Management of the Enclosed Coastal Seas 2018年11月 口頭発表（一般）
  • Land-ocean integrated management of Toyama Bay in the international semi enclosed sea, Japan Sea  [通常講演]
    Yoshida, T, Zhang, J, Morimoto, A, Shibano, R, Hirose, N, Takayama, T, Guo, X, Wang, Y, Mano, T
    The 12th International Conference on the Environmental Management of the Enclosed Coastal Seas 2018年11月 口頭発表（一般）
  • Simulation of river plume behaviors in a tropical region: Case study of the Upper Gulf of Thailand  [通常講演]
    Yu, X, Guo, X, Morimoto, A, Buranapratheprat, A
    The 12th International Conference on the Environmental Management of the Enclosed Coastal Seas 2018年11月 口頭発表（一般）
  • 豊後水道の内部潮汐  [通常講演]
    神田泰成, 郭新宇, 森本昭彦, 堤英輔
    2018年度日本海洋学会秋季大会 2018年09月 口頭発表（一般）
  • 若狭湾の水温変動と沖合の流動変動の関連性の検討  [通常講演]
    大西徹, 兼田淳史, 桂田慶裕, 森本昭彦, 伊藤雅
    2018年度日本海洋学会秋季大会 2018年09月 口頭発表（一般）
  • 2つの潮流調和定数の差の評価  [通常講演]
    滝川哲太郎, 森本昭彦, 千手智晴
    2018年度日本海洋学会秋季大会 2018年09月 口頭発表（一般）
  • 豊後水道の海洋物理現象  [通常講演]
    森本昭彦
    愛媛大学沿岸環境科学研究センター共同利用研究集会 豊後水道研究会 2018年08月 口頭発表（一般）
  • 豊後水道の底入り潮  [通常講演]
    森本昭彦, 浅原貫太, 前谷佳奈, 滝川哲太郎
    九州大学応用力学研究所共同利用研究集会 日本海及び日本周辺海域における環境急変現象（急潮）のモニタリング、モデリング及びメカニズム解明に関する研究集会 2018年08月 口頭発表（一般）
  • 山口県見島周辺海域を通過する対馬暖流沿岸分枝の流量推定  [通常講演]
    橋本涼介, 滝川哲太郎, 渡辺俊輝, 森本昭彦
    北海道大学低温科学研究所研究集会宗谷暖流を始めとした対馬暖流系の変動メカニズム 2018年07月 口頭発表（一般）
  • 対馬海峡を通過し日本海へ供給される栄養塩の起源  [通常講演]
    森本昭彦, 柴野良太, 高山勝巳, 伊藤雅, 滝川哲太郎
    北海道大学低温科学研究所研究集会宗谷暖流を始めとした対馬暖流系の変動メカニズム 2018年07月 口頭発表（一般）
  • 2nd branch of the Tsushima Warm Current path off San’in observed by ocean radar and satellite altimetry data  [通常講演]
    Morimoto,A, Sugitani, S, Amagai, J, Iwai, H, Kyushima, M, Takikawa, T, Ichikawa, K, Fujii, S
    The 4th Ocean Radar Conference for Asia-Pacific 2018年06月 口頭発表（一般）
  • 係留ADCP観測による豊後水道の底入り潮に関する研究  [通常講演]
    森本昭彦, 浅原貫太, 滝川哲太郎
    日本地球惑星科学連合2018大会 2018年05月 口頭発表（一般）

MISC

  • 2nd branch of the Tsushima Warm Current path off San’in observed by ocean radar and satellite altimetry data
    Morimoto, A, Sugitani, S, Amagai, J, Iwai, H, Kyushima, M, Takikawa, T, Ichikawa, K, Fujii, S Proceedings of The 4th Ocean Radar Conference for Asia-Pacific 記事・総説・解説・論説等（国際会議プロシーディングズ） 13 -16 2018年05月
  • 水産大学校練習船による対馬海峡における現場海洋観測
    滝川哲太郎, 森本昭彦, 鬼塚剛 海洋水産エンジニアリング 速報，短報，研究ノート等（学術雑誌） 128 68 -74 2016年07月
  • 非主要分潮が時刻固定のフェリー観測に与える影響について
    市川香, 元村和史, 岩清水堂徳, 森本昭彦, 福留研一, 尹宗煥 九州大学応用力学研究所所報 速報，短報，研究ノート等（大学，研究機関紀要） 146 137 -141 2014年
  • 対馬海峡における懸濁態有機窒素の季節変化と水平輸送量
    鬼塚剛, 渡邉敦, 森本昭彦, 滝川哲太郎, 杢雅利, 柳哲雄 九州大学応用力学研究所所報 速報，短報，研究ノート等（大学，研究機関紀要） 145 79 -82 2013年
  • The structure temperature-salinity and speed of sound in seawater in Danang-Quynhon area
    Tran, A. T, Le, D. C, Do, T. B, Morimoto, A, Yanagi, T Proc. of international cooperation on investigation and research of Marine natural resource and environment 記事・総説・解説・論説等（国際会議プロシーディングズ） 243 -250 2011年
  • Seasonal variation of sea surface current in the Gulf of Thailand
    S. Pramot, A. Morimoto, T. Yanagi Coastal Marine Science 34 (1) 91 -102 2010年09月
  • Interannual variation in nutrient transport through the Tsushima Strait
    Morimoto, A, Gotoh, A, Senjyu, T, Onitsuka, G, Takikawa, T, Watanabe, A, Moku, M Proc. of 5th PEACE Workshop 研究発表ペーパー・要旨（国際会議） 71 -74 2010年
  • Interannual variation in material transports through the eastern channel of the Tsushima/Korea Straits
    Morimoto, A, Watanabe, A, Takikawa, T, Onitsuka, G, Moku, M, Yanagi, T Proc. of 15th Pacific-Asian Marginal Seas Meeting 研究発表ペーパー・要旨（国際会議） 252 -255 2009年
  • Short-term periodic appearance of cold deeper water in subsurface layer of Sagami Bay, Japan
    Takahashi, D, Morimoto, A, Nakamura, T, Hosaka, T, Dang, V. H, Saino, T Proc. of 15th Pacific-Asian Marginal Seas Meeting 研究発表ペーパー・要旨（国際会議） 279 -282 2009年
  • Counterclockwise eddy downstream of Tsushima Islands estimated from hydrographic and ferryboat ADCP data
    Takikawa, T, Onitsuka, G, Fukudome, K, Yoon, J.-H, Moku, M, Morimoto, A, Watanabe, A Proc. of 15th Pacific-Asian Marginal Seas Meeting 研究発表ペーパー・要旨（国際会議） 283 -287 2009年
  • pCO2 distributions in the East China Sea-Japan Sea shelf estimated from climatological sea surface temperature, chlorophyll a and salinity
    Watanabe, A, Morimoto, A, Takikawa, T, Onitsuka, G, Saino, T Proceedings of the 14th PAMS/JECSS Workshop 研究発表ペーパー・要旨（国際会議） 68 -71 2007年
  • Observation of material transport through the eastern channel of the Tsushima/Korea Strait
    Morimoto, A, Onitsuka, G, Takikawa, T, Watanabe, A Proceedings of the 14th PAMS/JECSS Workshop 研究発表ペーパー・要旨（国際会議） 208 -209 2007年
  • Characteristics of water mass under the surface mixed layer in the Tsushima Straits
    Takikawa, T, Morimoto, A, Onitsuka, G, Watanabe, A, Moku, M Proceedings of the 14th PAMS/JECSS Workshop 研究発表ペーパー・要旨（国際会議） 210 -213 2007年
  • Characteristics of water mass in the eastern channel of the Tsushima Straits in early winter 2004
    Takikawa, T, Morimoto, A, Onitsuka, G, Mizutani, S, Hata, K, Ozono, H, Ikeda, T, Sakai, K. Kon Workshop on the Marine Environment in the East Asian Marginal Seas - Transport of materials -, Research Institute for Applied Mechanics, Kyushu University 研究発表ペーパー・要旨（国際会議） 109 -111 2005年
  • Cross section observation of physical, chemical and biological components in Eastern Channel of the Tsushima Strait
    Morimoto, A, Onitsuka, G, Takikawa, T, Watanabe, A, Mino, Y Workshop on the Marine Environment in the East Asian Marginal Seas - Transport of materials -, Research Institute for Applied Mechanics, Kyushu University 研究発表ペーパー・要旨（国際会議） 94 -96 2005年
  • Sea surface current in the Japan (East) Sea derived from satellite altimetric data
    Morimoto, A, Yanagi, T Proceedings of 11th PAMS/JECSS Meeting 研究発表ペーパー・要旨（国際会議） 105 -107 2001年
  • Sea surface circulation in the South China Sea derived from altimetric data of TOPEX/POSEIDON
    Morimoto, A, Yanagi, T, Yoshimoto, K Proceedings of the Tenth JSPS Joint Seminar on Marine and Fishery Sciences 記事・総説・解説・論説等（国際会議プロシーディングズ） 261 -271 1999年
  • Importance of tidal stress in the numerical model of residual flow in the coastal sea
    Yanagi, T, J. Yamamoto, A. Morimoto, M. Fujiwara Reports of Research Institute for Applied Mechanics, Kyushu University 速報，短報，研究ノート等（大学，研究機関紀要） 44 1 -10 1998年 [査読有り]
  • 黄海、東シナ海における海面高度計データの解析
    森本昭彦, 市川香, 柳哲雄 海面高度計データの海洋・固体地球研究への応用 報告書 会議報告等 143 -147 1996年

共同研究・競争的資金等の研究課題

  • 日本海環境変動予測モデルの構築
    環境省：環境研究総合推進費
    研究期間 : 2014年04月 -2019年03月 
    代表者 : 森本 昭彦
  • 河川流量変化に伴う北部タイランド湾の貧酸素水塊の挙動に関する研究
    日本学術振興会：(1) 科学研究費補助金 基盤研究(B)（海外学術調査）
    研究期間 : 2014年04月 -2017年03月 
    代表者 : 森本 昭彦
  • 遠距離海洋レーダを用いた対馬暖流の流路観測と流路分岐メカニズムの解明
    日本学術振興会：科学研究費補助金 基盤研究(A)
    研究期間 : 2013年04月 -2017年03月 
    代表者 : 森本 昭彦
  • 雲解像大気・海洋・波浪結合モデルによる台風強度推定
    文部科学省：気候変動リスク情報創生プログラム
    研究期間 : 2012年04月 -2017年03月 
    代表者 : 坪木和久
  • 窒素・リン比の時間・空間変化が東シナ海の物質循環へ与える影響
    日本学術振興会：科学研究費補助金 挑戦的萌芽研究
    研究期間 : 2013年04月 -2015年03月 
    代表者 : 森本 昭彦
  • 中国沿岸から日本海への物質輸送過程解明に向けた東シナ海・黄海表層流
    日本学術振興会：科学研究費補助金 基盤研究(B)
    研究期間 : 2010年04月 -2013年03月 
    代表者 : 森本 昭彦
  • 大型クラゲ国際共同調査委託事業
    水産庁：
    研究期間 : 2009年04月 -2013年03月 
    代表者 : 石坂丞二
  • 科学研究費補助金 特定領域研究
    日本学術振興会：
    研究期間 : 2006年04月 -2011年03月 
    代表者 : 齋藤誠一
  • 科学研究費補助金 特別研究院奨励費 外国人特別研究
    日本学術振興会：
    研究期間 : 2008年04月 -2010年03月 
    代表者 : 森本 昭彦
  • 人工衛星による海洋基礎生産モニタリング
    科学技術振興機構：戦略的創造研究推進事業 発展研究
    研究期間 : 2004年04月 -2009年03月 
    代表者 : 才野敏郎
  • 東シナ海から流入する大陸起源の淡水が日本海の熱塩循環に及ぼす影響
    日本学術振興会：科学研究費補助金 基盤研究(C)
    研究期間 : 2003年04月 -2006年03月 
    代表者 : 千手智晴

愛媛大学教員活動実績

教育活動(B)

担当授業科目(B01)

  • 2019, 前期, 学部, 海洋物理学Ⅰ
  • 2019, 前期, 学部, 沿岸海洋学
  • 2019, 前期, 学部, 地球科学野外研究
  • 2019, 前期, 学部, 海洋物理学
  • 2019, 前期, 修士, 地球科学高等実験Ⅰ
  • 2019, 前期, 修士, 地球科学高等実験Ⅴ
  • 2019, 前期, 修士, 地球科学フィールド高等実習Ⅰ
  • 2019, 前期, 修士, 地球科学フィールド高等実習Ⅲ
  • 2019, 前期, 修士, 地球科学プレゼンテーション特別実習Ⅰ
  • 2019, 前期, 修士, 地球科学プレゼンテーション特別実習Ⅲ
  • 2019, 前期, 修士, 地球科学ゼミナールⅠ
  • 2019, 前期, 修士, 地球科学プレゼンテーション特別実習Ⅱ
  • 2019, 前期, 修士, 地球科学フィールド高等実習Ⅱ
  • 2019, 前期, 修士, 地球科学高等実験Ⅲ
  • 2019, 前期, 学部, 海洋物理学Ｉ
  • 2019, 前期, 学部, 沿岸海洋学
  • 2019, 前期, 学部, 地球科学野外研究

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