Relevant bibliographies by topics / Japan Meteorology

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
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Academic literature on the topic 'Japan Meteorology'

Author: Grafiati
Published: 29 July 2024
Last updated: 31 July 2024

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Journal articles on the topic "Japan Meteorology"

1

Tsuda, T., K. Heki, S. Miyazaki, K. Aonashi, K. Hirahara, H. Nakamura, M. Tobita, et al. "GPS meteorology project of Japan —Exploring frontiers of geodesy—." Earth, Planets and Space 50, no. 10 (October 1998): i—v. http://dx.doi.org/10.1186/bf03352172.

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Khunai-ool, Chimis V., and Elena G. Gienko. "GNSS-METEOROLOGY: OPPORTUNITIES AND PROSPECTS FOR DEVELOPMENT IN RUSSIA AND ABROAD." Interexpo GEO-Siberia 6, no. 2 (July 8, 2020): 128–34. http://dx.doi.org/10.33764/2618-981x-2020-6-2-128-134.

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The article considers the possibilities and prospects for the development of GNSS meteorology based on domestic and foreign research. It is noted that the tropospheric delay of the GNSS signal is a valuable source of information about the state of the troposphere. The algorithm for estimating tropospheric delay and the services that perform this assessment (international GNSS service IGS and online service GAPS) are described. The content of the IGS output file with tropospheric delays at the IGS point is considered. The necessary conditions for the implementation of GNSS meteorology are listed, as well as structural diagrams of existing GNSS meteorology systems in the United States and Japan. It is shown that research in this area is being carried out in Russia. It is concluded that the network of permanent base stations in the Novosibirsk Region has the potential for the development of GNSS meteorology in the covered area.
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HOSHIKAWA, Kazutoshi, and Jun SUZUKI. "Local Meteorology and Agriculture on a Mountain-Slope in Central Japan." Journal of Agricultural Meteorology 60, no. 5 (2005): 853–56. http://dx.doi.org/10.2480/agrmet.853.

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Miyagawa, Takuya. "FOR 'CENTRES OF CALCULATIONS?’: 'COLONIAL METEOROLOGY’ IN NINETEENTH CENTURY JAPAN." Journal of Astronomical History and Heritage 26, no. 1 (March 1, 2023): 97–112. http://dx.doi.org/10.3724/sp.j.1440-2807.2023.01.06.

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Kurokawa, J., T. Ohara, I. Uno, M. Hayasaki, and H. Tanimoto. "Influence of meteorological variability on interannual variations of the springtime boundary layer ozone over Japan during 1981–2005." Atmospheric Chemistry and Physics Discussions 9, no. 2 (March 23, 2009): 7555–88. http://dx.doi.org/10.5194/acpd-9-7555-2009.

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Abstract. We investigated the influence of meteorological variability on the interannual variation of the springtime boundary layer ozone over Japan during 1981–2005 by multiyear simulations with the Models-3 Community Multiscale Air Quality (CMAQ) modeling system and the Regional Emission Inventory in Asia (REAS). CMAQ/REAS generally reproduced the observed interannual variability of springtime ozone over Japan, showing year-to-year variations larger than the annual rate of increase of the long-term trend. We then analyzed the influence of the interannual variation of meteorological fields in simulated results by using the fixed emissions for 2000 and meteorology data for each year. As a reference parameter, we calculated the area-weighted surface pressure anomaly over the Pacific Ocean east of Japan. When the anomaly has a large negative value, polluted air masses from continental Asia tend to be transported directly to Japan by westerly winds. In contrast, when the anomaly has a large positive value, the influences of the outflow from continental Asia tends to be small because the westerly components of wind fields around Japan are comparatively weak. Instead, southerly winds are relatively strong and transport clean air masses from the Pacific Ocean to Japan. Consequently, springtime ozone over Japan is higher (lower) than in ordinary years when the anomaly has a large negative (positive) value. In general, the interannual variation of springtime ozone over Japan is sensitive to the outflow from continental Asia. We also found some correlation between springtime ozone over Japan and the El Niño-Southern Oscillation, indicating that higher and lower springtime ozone over Japan are related to La Niña and El Niño, respectively. Differences in the meridional displacement and diversity of cyclone tracks near Japan between El Niño and La Niña years may be responsible for interannual variations in the springtime boundary layer ozone over Japan.
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Kurokawa, J., T. Ohara, I. Uno, M. Hayasaki, and H. Tanimoto. "Influence of meteorological variability on interannual variations of springtime boundary layer ozone over Japan during 1981–2005." Atmospheric Chemistry and Physics 9, no. 17 (September 1, 2009): 6287–304. http://dx.doi.org/10.5194/acp-9-6287-2009.

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Abstract. We investigated the influence of meteorological variability on the interannual variation of springtime boundary layer ozone over Japan during 1981–2005 by multiyear simulations with the Models-3 Community Multiscale Air Quality (CMAQ) modeling system and the Regional Emission Inventory in Asia (REAS). CMAQ/REAS generally reproduced the observed interannual variability of springtime ozone over Japan, showing year-to-year variations larger than the annual rate of increase of the long-term trend. We then analyzed the influence of the interannual variation of meteorology in simulated results by using the fixed emissions for 2000 and meteorological fields for each year. As a reference parameter, we calculated the area-weighted surface pressure anomaly over the Pacific Ocean east of Japan. When the anomaly has a large negative value, polluted air masses from continental Asia tend to be transported directly to Japan by westerly winds. In contrast, when the anomaly has a large positive value, influence of the outflow from continental Asia tends to be small because the westerly components of wind fields around Japan are comparatively weak. Instead, southerly winds are relatively strong and transport clean air masses from the Pacific Ocean to Japan. Consequently, springtime ozone over Japan is higher (lower) than in ordinary years when the anomaly has a large negative (positive) value. In general, the interannual variation of springtime ozone over Japan is sensitive to the outflow from continental Asia. We also found some correlation between springtime ozone over Japan and the El Niño-Southern Oscillation, indicating that higher and lower springtime ozone over Japan are related to La Niña and El Niño, respectively. Differences in the meridional displacement and diversity of cyclone tracks near Japan between El Niño and La Niña years may be responsible for interannual variations in the springtime boundary layer ozone over Japan.
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7

Feklova, Tatiana. "The History of Organization of the International System of Magnetic and Meteorological Observations in the Second Half of the 19th Century." Voprosy istorii estestvoznaniia i tekhniki 44, no. 1 (2023): 79. http://dx.doi.org/10.31857/s020596060024497-8.

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The article deals with some little-studied pages from the history of the development of international cooperation in the field of meteorology. With climate being a transboundary phenomenon, the international cooperation of researchers who studied it was a natural process. The first attempts to create an international network of meteorological stations date back to the mid-18th century. The article offers unique data about the distribution of meteorological stations by countries in the mid-19th century. The author looks into the stages in the development of the international network of meteorological stations and observatories. Special attention is given to the role of the Main Physical Observatory, and the scientists who worked there – first and foremost, the Observatory’s Director, Heinrich von Wild (Genrikh Ivanovich Vilʼd) – in the formation and evolution of this network. An important event in the development of meteorology was the 1st Meteorological Congress held in Vienna in 1873. One of the outcomes of this congress was creation of the Permanent Meteorological Committee. After the 2nd International Meteorological Congress held in Rome in 1879, the International Meteorological Committee was set up to replace the Permanent Meteorological Committee. Heinrich von Wild was appointed its President. The IMC’s goals were promoting and coordinating the work of meteorologists around the world. After some modernization, the committee has existed up to this day. The article offers the data on the contacts between Russia and other countries such as the UK, the USA, and Japan in the field of meteorology. Thus, as a result of the development of contacts between Russia and the UK, a magnetic and meteorological observatory was set up in Novo-Arkhangelsk (now Sitka, Alaska). This article is based on the archival records from the Russian State Archive of the Navy.
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Zikra, Muhammad, Noriaki Hashimoto, Kodama Mitsuyasu, Trika Pitana, and Silvianita. "Seasonally Variation of Significant Wave Height for 25 Year Period Based on JMA/MRI-AGCM3.2 Wind Climate Data." Applied Mechanics and Materials 862 (January 2017): 67–71. http://dx.doi.org/10.4028/www.scientific.net/amm.862.67.

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The global ocean wave climate has long been of interest to the ocean engineering community because of the need for accurate operational wave data for applications such as vessel design, design of offshore and coastal structures or naval operations. Recently, there has been a major interest in wave climate changes as a result of global warming. Therefore, studies on predicting the effect of global warming on ocean wave climate are required. The objectives of this study are to analyze the accuracy and variability of global significant wave height hindcast for the 25 year period 1979-2003. This study describes the 25 year global significant wave height simulation derived from the Japan Meteorology Agency/Meteorology Research Institute (JMA/MRI)-AGCM3.2 wind climate data. The wind climate data were input into ocean wave model WAM with a global grid of spacing 1o in latitude by 1o in longitude. In situ wind and wave data sets from National Data Buoy Center (NDBC)-National Oceanic and Atmospheric Administration (NOAA) database were used to evaluate the hindcast accuracy. The validation showed good agreement both wind and waves data. The wave hindcast analysis show that the seasonal variability of significant wave height in the Northern Hemisphere is greater than in the Southern Hemisphere. Meanwhile, most of the equatorial regions are in calm condition all year.
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Gavrilov, N. M., S. Fukao, and T. Nakamura. "Gravity wave intensity and momentum fluxes in the mesosphere over Shigaraki, Japan (35°N, 136°E) during 1986-1997." Annales Geophysicae 18, no. 7 (July 31, 2000): 834–43. http://dx.doi.org/10.1007/s00585-000-0834-z.

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Abstract. Averaged seasonal variations of wind perturbation intensities and vertical flux of horizontal momentum produced by internal gravity waves (IGWs) with periods 0.2-1 h and 1-6 h are studied at the altitudes 65-80 km using the MU radar measurement data from the middle and upper atmosphere during 1986-1997 at Shigaraki, Japan (35° N, 136° E). IGW intensity has maxima in winter and summer, winter values having substantial interannual variations. Mean wave momentum flux is directed to the west in winter and to the east in summer, opposite to the mean wind in the middle atmosphere. Major IGW momentum fluxes come to the mesosphere over Shigaraki from the Pacific direction in winter and continental Asia in summer.Key words: Meteorology and atmospheric dynamics (middle atmosphere dynamics; waves and tides) · Ionosphere (ionospheric disturbances)
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Sato, Kazutoshi, Eugenio Realini, Toshitaka Tsuda, Masanori Oigawa, Yuya Iwaki, Yoshinori Shoji, and Hiromu Seko. "A High-Resolution, Precipitable Water Vapor Monitoring System Using a Dense Network of GNSS Receivers." Journal of Disaster Research 8, no. 1 (February 1, 2013): 37–47. http://dx.doi.org/10.20965/jdr.2013.p0037.

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This work describes a system aimed at the near realtimemonitoring of precipitable water vapor (PWV) by means of a dense network of Global Navigation Satellite System (GNSS) receivers. These receivers are deployed with a horizontal spacing of 1-2 km around the Uji campus of Kyoto University, Japan. The PWV observed using a standard GPS meteorology technique, i.e., by using all satellites above a low elevation cutoff, is validated against radiosonde and radiometer measurements. The result is a RMS difference of about 2 mm. A more rigorous validation is done by selecting single GPS slant delays as they pass close to the radiosonde or the radiometer measuring directions, and higher accuracy is obtained. This method also makes it possible to preserve short-term fluctuations that are lost in the standard technique due to the averaging of several slant delays. Geostatistical analysis of the PWV observations shows that they are spatially correlated within the area of interest; this confirms that such a dense network can detect inhomogeneous distributions in water vapor. The PWV horizontal resolution is improved by using high-elevation satellites only, with the aim of exploiting at best the future Quasi-Zenith Satellite System (QZSS), which will continuously provide at least one satellite close to the zenith over Japan.
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Dissertations / Theses on the topic "Japan Meteorology"

1

Shinohara, Aya. "Competition Among Juvenile Acropora on Shallow Reefs, Okinawa, Japan." NSUWorks, 2004. http://nsuworks.nova.edu/occ_stuetd/273.

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The processes structuring coral communities involve many factors including recruitment dynamics, competitive interactions, and acute and chronic disturbances. The shallow reef at Sunabe (Okinawa, Ryukyu Islands, Japan) was dominated by a dense cover of mainly Acropora spp. until the bleaching event in 1998, when most colonies died. Subsequent monitoring of the community showed that the number of juvenile colonies was high in 2000 and competition among these colonies may affect community dynamics. The aim of this study was to determine the possibility of predicting community change and recovery, using short-term observation data of size-specific mortality and growth rates of coral recruits. Predictions were made using a demographic model based on a Leslie-matrix approach with data collected on the shallow reefs of Sunabe in 2000. This existing data showed a tendency of high mortality of competing colonies, but with no significant difference among species. Over the period of 2000-2004 percent cover of Acropora sp. increased from 16% to 22% however the number of colonies decreased (from 6.5 per quadrat to 2.5 per quadrat). The prediction of size fraction derived from the matrix population model and the observed size fraction based on the 2004 data showed some agreement; however the model predicted a high number of colonies in the largest size class. There were no adult colonies in 2000. A known bleaching event in 2002, causing mortality of reproducing adult colonies (high mortality and low growth rates) is most probably the reason for the disagreement between is the matrix model-based prediction and the observed community structure. Therefore, it is suggested that one more size class is add to the model, representing reproducing colonies. It is also suggested that further improvement of the model is needed for disturbances (such as bleaching, typhoon, and mass predation events). Despite these suggested improvements, the model presented here shows that it is possible to use simple community data taken over the course of 1 year to predict short-term community size class dynamics and population growth on juvenile Acropora spp. dominated reefs. Thus, such investigations have practical value for the management of coral resources.
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Books on the topic "Japan Meteorology"

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Tokyo, Japan) Meeting on Asia-Pacific Satellite Data Utilization and Exchange (1999. Proceedings of Meeting on Asia-Pacific Satellite Data Utilization and Exchange,Tokyo, Japan, 2-4 February 1999. Tokyo]: Japan Meteorological Agency, 1999.

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(Japan), Kishō Eisei Sentā. Sōritsu 25-nenshi: Kishō Eisei Sentā. Kiyose-shi: Kishō Eisei Sentā, 2002.

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Yoshida, Tsunao. Yasen Kishō Daigo Daitai Daiichi Chūtai, Daini Kishō Rentai Daigo Chūtai, Daijūshi Yasen Kishōtai Daigo Chūtai taishi: Aru kishō chūtai no kiseki. [Tokyo: Yoshida Tsunao], 1988.

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(Japan), Kishō Kenkyūjo. Kishō Kenkyūjo zōsho mokuroku: Tsuiroku : Library catalogue of Meteorological Research Institute. Ibaraki-ken Tsukuba-shi: Kishōchō Kishō Kenkyūjo, 1988.

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International Workshop on GPS Meteorology (2003 Tsukuba, Japan). Application of GPS remote sensing to meteorology and related fields: A collection of papers presented at the International Workshop on GPS Meteorology : GPS meteorology: ground-based and space-borne applications : 14-17 Jan. 2003, Tsukuba, Japan. Tokyo, Japan: Meteorological Society of Japan, 2004.

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International, Workshop for Advanced Flux Network and Flux Evaluation (2000 Sapporo Japan). International Workshop for Advanced Flux Network and Flux Evaluation, 27-29 September 2000, Hokkaido University, Sapporo, Japan. Ibaraki, Japan: Center for Global Environmental Research, National Institute for Environmental Studies, 2001.

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International Symposium on Assimilation of Observations in Meteorology and Oceanography (2nd 1995 Tokyo, Japan). Data assimilation in meteorology and oceanography: Theory and practice : a collection of papers presented at the WMO Second International Symposium on Assimilation of Observations in Meteorology and Oceanography, 13-17 March 1995, Tokyo, Japan. Tokyo: Meteorological Society of Japan, 1997.

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Joint Scientific & Technical Committee for GCOS. Report of the fifth session of the Joint Scientific & Technical Committee for GCOS: Hakone, Japan, October 16-19, 1995. Geneva: Joint Planning Office, Global Climate Observing System, 1995.

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United States. Department of State, ed. Satellites: Agreement between the United States of America and Japan, effected by exchange of notes at Washington, February 18, 2005, with implementing arrangement. Washington, D.C.]: U.S. Dept. of State, 2012.

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Panel, GCOS/GOOS/GTOS Joint Data and Information Management. Report of the GCOS/GOOS/GTOS Joint Data and Information Management Panel: Third session, Tokyo, Japan, 15-18 July 1997. Geneva: Joint Planning Office, Global Climate Observing System, 1997.

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Book chapters on the topic "Japan Meteorology"

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Kodaira, Nobuhiko, and Jiro Aoyagi. "History of Radar Meteorology in Japan." In Radar in Meteorology, 69–76. Boston, MA: American Meteorological Society, 1990. http://dx.doi.org/10.1007/978-1-935704-15-7_9.

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"Weathering Fuji: Marriage, Meteorology, and the Meiji Bodyscape." In Japan at Nature's Edge, 152–74. University of Hawaii Press, 2017. http://dx.doi.org/10.1515/9780824838775-011.

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Conference papers on the topic "Japan Meteorology"

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Sasa, Kenji, Chen Chen, Shigeaki Shiotani, Teruo Ohsawa, and Daisuke Terada. "Numerical Analysis of Failed Forecasts of Waves Under Low Pressures From Viewpoint of Ship Operation." In ASME 2014 33rd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/omae2014-23876.

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Today, weather routing becomes more important under the current situation of international maritime transportation. However, the authors reveal that the current systems are not necessarily sufficiently reliable. It is also worthwhile to consider the background of the difficulty in numerically forecasting winds and waves. Here, two failed cases of wave forecasts are verified using WRF and SWAN, two numerical meso-meteorology models. In both failed cases, low pressures developed from the southern sea area of Japan with a northeast direction. First, wind direction can be reproduced correctly, even if the resolution of the simulation is changed. Second, if the resolution is insufficient, wind speed will be underestimated as smaller than the observed values. At the same time, wave height tends to be underestimated as compared to observed values, too. This is the feasibility study for improving the forecasting of wave growth pattern due to developing low pressures from the viewpoint of safe ship operation.
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Reports on the topic "Japan Meteorology"

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Friehe, Carl A. Japan/East Sea Air-Sea Interaction and Meteorology: Boundary-Layer Structure and Model Validation. Fort Belvoir, VA: Defense Technical Information Center, September 2000. http://dx.doi.org/10.21236/ada610245.

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Friehe, Carl A., and Djamal Khelif. Japan/East Sea Air-Sea Interaction and Meteorology: Boundary-Layer Structure and Model Validation. Fort Belvoir, VA: Defense Technical Information Center, August 2001. http://dx.doi.org/10.21236/ada625707.

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Friehe, Carl A., and Djamal Khelif. Japan/East Sea Air-Sea Interaction and Meteorology: Boundary-Layer Structure and Model Validation. Fort Belvoir, VA: Defense Technical Information Center, September 2002. http://dx.doi.org/10.21236/ada626447.

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