View Oirase’S Fresh Greenery in Spring and the Changing Colors of Tsutanuma in Autumn
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PICES Sci. Rep. No. 2, 1995
TABLE OF CONTENTS Page FOREWORD vii Part 1. GENERAL INTRODUCTION AND RECOMMENDATIONS 1.0 RECOMMENDATIONS FOR INTERNATIONAL COOPERATION IN THE OKHOTSK SEA AND KURIL REGION 3 1.1 Okhotsk Sea water mass modification 3 1.1.1Dense shelf water formation in the northwestern Okhotsk Sea 3 1.1.2Soya Current study 4 1.1.3East Sakhalin Current and anticyclonic Kuril Basin flow 4 1.1.4West Kamchatka Current 5 1.1.5Tides and sea level in the Okhotsk Sea 5 1.2 Influence of Okhotsk Sea waters on the subarctic Pacific and Oyashio 6 1.2.1Kuril Island strait transports (Bussol', Kruzenshtern and shallower straits) 6 1.2.2Kuril region currents: the East Kamchatka Current, the Oyashio and large eddies 7 1.2.3NPIW transport and formation rate in the Mixed Water Region 7 1.3 Sea ice analysis and forecasting 8 2.0 PHYSICAL OCEANOGRAPHIC OBSERVATIONS 9 2.1 Hydrographic observations (bottle and CTD) 9 2.2 Direct current observations in the Okhotsk and Kuril region 11 2.3 Sea level measurements 12 2.4 Sea ice observations 12 2.5 Satellite observations 12 Part 2. REVIEW OF OCEANOGRAPHY OF THE OKHOTSK SEA AND OYASHIO REGION 15 1.0 GEOGRAPHY AND PECULIARITIES OF THE OKHOTSK SEA 16 2.0 SEA ICE IN THE OKHOTSK SEA 17 2.1 Sea ice observations in the Okhotsk Sea 17 2.2 Ease of ice formation in the Okhotsk Sea 17 2.3 Seasonal and interannual variations of sea ice extent 19 2.3.1Gross features of the seasonal variation in the Okhotsk Sea 19 2.3.2Sea ice thickness 19 2.3.3Polynyas and open water 19 2.3.4Interannual variability 20 2.4 Sea ice off the coast of Hokkaido 21 -
The Kuroshio Extension: a Leading Mechanism for the Seasonal Sea-Level Variability Along the West
1 The Kuroshio Extension: A Leading Mechanism for the Seasonal Sea-level Variability along the West 2 Coast of Japan 3 4 Chao Ma1, 2, 3, Jiayan Yang3, Dexing Wu2, Xiaopei Lin2 5 6 1. College of Physical and Environmental Oceanography 7 Ocean University of China 8 Qingdao 266100, China 9 2. Physical Oceanography Laboratory 10 Ocean University of China 11 Qingdao 266100, China 12 3. Department of Physical Oceanography 13 Woods Hole Oceanographic Institution 14 Woods Hole, MA 02543, USA 15 16 Corresponding Author: Chao Ma ([email protected]) 17 Abstract 18 Sea level changes coherently along the two coasts of Japan on the seasonal time scale. AVISO 19 satellite altimetry data and OFES (OGCM for the Earth Simulator) results indicate that the variation 20 propagates clockwise from Japan's east coast through the Tsushima Strait into the Japan/East Sea (JES) 21 and then northward along the west coast. In this study, we hypothesize and test numerically that the sea 22 level variability along the west coast of Japan is remotely forced by the Kuroshio Extension (KE) off the 23 east coast. Topographic Rossby waves and boundary Kelvin waves facilitate the connection. Our 3-d 24 POM model when forced by observed wind stress reproduces well the seasonal changes in the vicinity 25 of JES. Two additional experiments were conducted to examine the relative roles of remote forcing and 26 local forcing. The sea level variability inside the JES was dramatically reduced when the Tsushima Strait 27 is blocked in one experiment. The removal of the local forcing, in another experiment, has little effect on 28 the JES variability. -
Scouting, Signaling, and Gatekeeping: Chinese Naval
U.S. NAVAL WAR COLLEGE CHINA MARITIME STUDIES Number 2 Scouting, Signaling, and Gatekeeping Chinese Naval Operations in Japanese Waters and the International Law Implications ISBN: 978-1-884733-60-4 Peter Dutton 9 781884 733604 Scouting, Signaling, and Gatekeeping Chinese Naval Operations in Japanese Waters and the International Law Implications Peter Dutton CHINA MARITIME STUDIES INSTITUTE U.S. NAVAL WAR COLLEGE NEWPORT, RHODE ISLAND www.usnwc.edu/cnws/cmsi/default.aspx Naval War College The China Maritime Studies are extended research projects Newport, Rhode Island that the editor, the Dean of Naval Warfare Studies, and the Center for Naval Warfare Studies President of the Naval War College consider of particular China Maritime Study No. 2 interest to policy makers, scholars, and analysts. February 2009 Correspondence concerning the China Maritime Studies may be addressed to the director of the China Maritime President, Naval War College Studies Institute, www.usnwc.edu/cnws/cmsi/default.aspx. Rear Admiral James P. Wisecup, U.S. Navy To request additional copies or subscription consideration, Provost please direct inquiries to the President, Code 32A, Naval Amb. Mary Ann Peters War College, 686 Cushing Road, Newport, Rhode Island 02841-1207, or contact the Press staff at the telephone, fax, Dean of Naval Warfare Studies or e-mail addresses given. Robert C. Rubel Reproduction and printing is subject to the Copyright Act Director of China Maritime Studies Institute of 1976 and applicable treaties of the United States. This Dr. Lyle J. Goldstein document may be freely reproduced for academic or other noncommercial use; however, it is requested that Naval War College Press reproductions credit the author and China Maritime Director: Dr. -
Effects of Eddy Variability on the Circulation of the Japan/ East Sea
Journal of Oceanography, Vol. 55, pp. 247 to 256. 1999 Effects of Eddy Variability on the Circulation of the Japan/ East Sea 1 1 2 G. A. JACOBS , P. J. HOGAN AND K. R. WHITMER 1Naval Research Laboratory, Stennis Space Center, Mississippi, U.S.A. 2Sverdrup Technology, Inc., Stennis Space Center, Mississippi, U.S.A. (Received 5 October 1998; in revised form 17 November 1998; accepted 19 November 1998) The effect of mesoscale eddy variability on the Japan/East Sea mean circulation is Keywords: examined from satellite altimeter data and results from the Naval Research Laboratory ⋅ Japan Sea, Layered Ocean Model (NLOM). Sea surface height variations from the Geosat-Exact ⋅ eddies, ⋅ altimeter, Repeat Mission and TOPEX/POSEIDON altimeter satellites imply geostrophic velocities. ⋅ At the satellite crossover points, the total velocity and the Reynolds stress due to numerical model- ing, geostrophic mesoscale turbulence are calculated. After spatial interpolation the momentum ⋅ Reynolds stress. flux and effect on geostrophic balance indicates that the eddy variability aids in the transport of the Polar Front and the separation of the East Korean Warm Current (EKWC). The NLOM results elucidate the impact of eddy variability on the EKWC separation from the Korean coast. Eddy variability is suppressed by either increasing the model viscosity or decreasing the model resolution. The simulations with decreased eddy variability indicate a northward overshoot of the EKWC. Only the model simulation with sufficient eddy variability depicts the EKWC separating from the Korean coast at the observed latitude. The NLOM simulations indicate mesoscale influence through upper ocean–topographic coupling. 1. Introduction Lie et al., 1995). -
Hachinohe Martial Arts Center About 15 Min
Access A Maeda Arena About 35 min. by car from Aomori Airport (New Aomori Prefecture Sports Park) About 25 min. by car from Shin-Aomori Station (JR Tohoku Shinkansen Line/Ou Line) B Michinokubank Dream Stadium About 30 min. by car from Aomori Airport (Aomori City Sports Complex) About 15 min. by car from Shin-Aomori Station (JR Tohoku Shinkansen Line/Ou Line) C Aomori Martial Arts Hall About 50 min. by car from Aomori Airport Hirosaki Athletic Park About 10 min. by car from Hirosaki Station (JR Ou Line/Konan Railway Konan Line) About 70 min. by car from Aomori Airport Mt. Iwakisan Synthesis Park About 40 min. by car from Hirosaki Station (JR Ou Line/Konan Railway Konan Line) D The right choice to train About 70 min. by car from Aomori Airport Iwaki Seishonen Sports Center About 45 min. by car from Hirosaki Station (JR Ou Line/Konan Railway Konan Line) AOMORI E About 70 min. by car from Aomori Airport Iwaki River Canoe Center About 30 min. by car from Hirosaki Station (JR Ou Line/Konan Railway Konan Line) About 55 min. by car from Misawa Airport Takamori Yama Sports Park About 30 min. by car from Shichinohe-Towada Station (JR Tohoku Shinkansen Line) F About 45 min. by car from Misawa Airport Towada City Wakaba Stadium About 25 min. by car from Shichinohe-Towada Station (JR Tohoku Shinkansen Line) About 40 min. by car from Misawa Airport Hachinohe Martial Arts Center About 15 min. by car from Hachinohe Station (JR Tohoku Shinkansen Line/Hachinohe Line/Aoimori Railway Line) G About 50 min. -
Historical Fish Specimens Collected from the Tohoku District by the Saito Ho-On Kai Museum of Natural History
Bull. Natl. Mus. Nat. Sci., Ser. A, 35(1), pp. 9–54, March 22, 2009 Historical Fish Specimens Collected from the Tohoku District by the Saito Ho-on Kai Museum of Natural History Keiichi Matsuura1, Gento Shinohara2 and Masanori Nakae1 1 Collection Center, National Museum of Nature and Science, 3–23–1 Hyakunin-cho, Shinjuku-ku, Tokyo, 169–0073 Japan E-mail: [email protected]; [email protected] 2 Department of Zoology, National Museum of Nature and Science, 3–23–1 Hyakunin-cho, Shinjuku-ku, Tokyo, 169–0073 Japan E-mail: [email protected] Abstract The fish collection of the Saito Ho-on Kai Museum of Natural History was transferred to the National Museum of Nature and Science, Tokyo in February 2006. Ninety percent of the fish collection contains specimens collected from the Tohoku District during the period from 1930 to 1933 when natural environments of Japan were in good condition for various groups of fishes. The fish specimens from the Tohoku District were classified into 361 species/subspecies of 273 genera belonging to 131 families of 31 orders. A list of the species is shown with remarks on distribution. Key words: Fish specimens, Saito Ho-on Kai Museum, Tohoku District, inventory. stead of natural sicence. The museum has tried to Introduction keep its activity at the level before the war, but it The Saito Ho-on Kai Museum was established failed to do so because of financial difficulties. In in November 1933 in Sendai City, Miyagi Pre- 2005, the Saito Ho-on Kai Museum of Natural fecture, Japan. -
Wine, Beer, Whisky, Etc
Current as of January 1, 2021 Compiled by Sendai Regional Taxation Bureau Brewery Excludes breweries listed on the Aomori Wine, Beer, "Aomori Brewery MAP (SAKE)". MAP whisky, etc. However, breweries that produce continuously distilled shochu (New type or shochu group Ko), specialty shochu (Authentic type or shochu group Otsu), and beer are listed in duplicate. Legend ㉑ 279 Shinkansen Kazamaura JR Line Oma Private Railway Town Village Expressway Major National Highway City Boundary Sai Shinkansen Station JR and Private Railway Stations Village Higashidoori Mutsu City Village Ominato Station Shimokita Station 279 Ominato Line Imabetsu 338 ⑳ Town Sotogahama Town Nakadomari Okutsugaru-Imabetsu Station Town 338 Sotogahama Yokohama Goshogawara TsugaruTown Line Town City Kanita Station Yomogita Nakadomari Village Town Hokkaido Shinkansen Rokkasho 339 280 ①② Village 4 Noheji ⑲ Goshogawara Aomori Port Station Tsugaru City Hiranai Town City Shin-Aomori Aomori Station Noheji Town Tohoku Ajigasawa Station 101 Goshogawara Town Station Aoimori Railway394 Line Station Ou Misawa Main 103 4 Line Shichinohe-Towada City Tsuruta 338 Town ⑰ Aomori Airport Station Itayanagi Shichinohe Misawa Airport Itayanagi Town Namioka Station Aomori City Town Tohoku Shinkansen Station 394 Misawa Station Ajigasawa Town Fujisaki Kuroishi Kawabe Station Town Station 394 Oirase Town Fukaura Station Hirosaki Inakadate Hachinohe Port City ④ VillageKonan ③ Railway Kuroishi 102 Rokunohe 45 Gono Line Fukaura ⑤ City Hon- ⑯ ⑦ Hiraka 4 Town Town Towada City ⑱ Hachinohe Same Station ⑧ Station Station ⑪ ⑨ 454 Hachinohe Hirosaki Station Station ⑬ Mutsu-Minato Station Nishimeya Hirakawa Hachinohe Line Village Gonohe Town Owani⑫ City 454 ⑥⑩ Town ⑮ 7 282 Shingo Village ⑭ Hashikami Nanbu Hachinohe Town Town City Sannohe Town Name of City, Town, and Village No. -