参考論文リスト

ヒマラヤ観測・メガラヤ観測(氷河・気象・水文等):

• Barros, A. P., Joshi, M., Putkonen, J., & Burbank, D. W. (2000), A study of the 1999 monsoon rainfall in a mountainous region in central Nepal using TRMM products and rain gauge observations. Geophysical Research Letters, 27, 3683–3686. https://doi.org/10.1029/2000GL011827 (ネパールヒマラヤ、最多雨領域での本格的な現地観測と衛星搭載降雨レーダデータとのマッチアップなど)

• Barros, A. P., & Lang, T. J. (2003), Monitoring the Monsoon in the Himalayas: Observations in central Nepal, June 2001. Monthly Weather Review, 131, 1408–1427. https://doi.org/10.1175/1520-0493(2003)131%3C1408:MTMITH%3E2.0.CO;2

• Ouyang, L., Yang, K., Lu, H., Chen, Y., Zhou, X., & Wang, Y. (2020). Ground-based observations reveal unique valley precipitation patterns in the Central Himalaya. Journal of Geophysical Research: Atmospheres, 125, e2019JD031502. (ヒマラヤ・雨量計観測・日変化・季節変化)

• Salerno, F., Guyennon, N., Thakuri, S., Viviano, G., Romano, E., Vuillermoz, E., et al. (2015). Weak precipitation, warm winters and springs impact glaciers of south slopes of Mt. Everest (central Himalaya) in the last 2 decades (1994–2013). The Cryosphere, 9, 1229–1247. https://doi.org/10.5194/tc-9-1229-201

• Shea, J. M., Wagnon, P., Immerzeel, W. W., Biron, R., Brun, F., & Pellicciotti, F. (2015), A comparative high-altitude meteorological analysis from three catchments in the Nepalese Himalaya. International Journal of Water Resources Development, 31, 174–200. https://doi.org/10.1080/07900627.2015.1020417. (ランタンのYala氷河とその周辺における通年気象観測. 氷河周辺の気象要素の特徴がまとめてある)

• Seppyo関連の特集号(1976）https://www.jstage.jst.go.jp/browse/seppyo/38/Special/_contents/-char/ja

• Sunako, S., Fujita, K., Sakai, A., & Kayastha, R. B. (2019). Mass balance of Trambau glacier, Rolwaling region, Nepal Himalaya: In-si-tu observations, long-term reconstruction and mass-balance sensitivity. Journal of Glaciology, 65, 605–616. https://doi.org/10.1017/jog.2019.37（ヒマラヤ・AWS・観測)

• Terao, T., Islam, M. N., Hayashi, T., & Oka, T. (2006). Nocturnal jet and its effects on early morning rainfall peak over northeastern Bangla-desh during the summer monsoon season. Geophysical Research Letters, 33, L18806. https://doi.org/10.1029/2006GL026156(メガラヤ・日変化・夜間ジェット)

• Ueno K., R.B. Kayastha, M. R. Chitrakar, O. R. Bajracharya, A. P. Pokhrel, H. Fujinami, T. Kadota, H.Iida, D.P. Manandhar, M. Hattori, T. Yasunari and M. Nakawo, 2001: Meteorological observations during 1994-2000 at the Automatic Weather Station (GEN-AWS) in Khumbu region, Nepal Himalayas. Bulletin of Glaciological Research, 18, 23-30.[Abstract][PDF]©Japanese Society of Snow and Ice (ヒマラヤ・クンブ・AWS・長期気象観測)

• Ueno, K., K. Toyotsu, L. Bertolani, and G. Tartari, 2008: Stepwise Onset of Monsoon Weather Observed in the Nepal Himalaya. Mon. Wea. Rev., 136, 2507–2522, https://doi.org/10.1175/2007MWR2298.1 (ヒマラヤ・クンブ・AWS・季節変化・日変化)

• Yang, K., Guyennon, N., Ouyang, L., Tian, L. D., Tartari, G., & Salerno, F. (2018). Impact of summer monsoon on the elevation-depend-ence of meteorological variables in the south of central Himalaya. International Journal of Climatology, 38, 1748–1759. https://doi.org/10.1002/joc.5293

• 藤井理行・安成哲三 (1983), ヒマラヤの気候と氷河, 気象学のプロムナード. (絶版になっている気象学のプロムナードシリーズの一冊。今のようなAWS(自動気象観測装置)のない時代、雨季も含めて現地滞在し観測した結果を基に構成されている。未だにヒマラヤでは、これを超える現地の気象観測はないと思う。実行力と結果に対する洞察は素直にすごい）

降水特性・衛星降水(TRMM, GPM, IMERG等):

• Barros, A. P., Kim, G., Williams, E., & Nesbitt, S. W. (2004), Probing orographic controls in the Himalayas during the monsoon using satellite imagery. Natural Hazards and Earth System Sciences, 4, 29–51. https://doi.org/10.5194/nhess-4-29-2004 .

• Bhatt, B.C. and K. Nakamura, 2005: Characteristics of Monsoon Rainfall around the Himalayas Revealed by TRMM Precipitation Radar. Mon. Wea. Rev., 133, 149–165, https://doi.org/10.1175/MWR-2846.1

• Bhatt, B. C., and Nakamura, K. ( 2006), A climatological‐dynamical analysis associated with precipitation around the southern part of the Himalayas, J. Geophys. Res., 111, D02115, doi:10.1029/2005JD006197.

• Bookhagen, B., and Burbank, D. W. ( 2006), Topography, relief, and TRMM‐derived rainfall variations along the Himalaya, Geophys. Res. Lett., 33, L08405, doi:10.1029/2006GL026037. (降水, TRMM, 地形, ダブルバンド)

• Bookhagen, B. (2010). Appearance of extreme monsoonal rainfall events and their impact on erosion in the Himalaya. Geomatics, Natural Hazards and Risk, 1, 37–50. https://doi.org/10.1080/1947570100362573

• Fujinami, H., Fujita, K., Takahashi, N., Sato, T., Kanamori, H., Sunako, S., & Kayastha, R. B. (2021). Twice-daily monsoon precipitation maxima in the Himalayas driven by land surface effects. Journal of Geophysical Research: Atmospheres, 126, e2020JD034255. https://doi.org/10.1029/2020JD034255(ヒマラヤ・日変化・地点雨量・TRMM)

• Hirose, M., R. Oki, S. Shimizu, M. Kachi, and T. Higashiuwatoko, 2008: Finescale Diurnal Rainfall Statistics Refined from Eight Years of TRMM PR Data. J. Appl. Meteor. Climatol., 47, 544–561, https://doi.org/10.1175/2007JAMC1559.1 （TRMM-PR, 全球, 日変化)

• Hirose, M. and K. Okada, 2018: A 0.01° Resolving TRMM PR Precipitation Climatology. J. Appl. Meteor. Climatol., 57, 1645–1661, https://doi.org/10.1175/JAMC-D-17-0280. 1 （TRMM-PR, 0.01度格子, 気候値）

• Houze, R. A., Wilton, D. C. and Smull, B. F. (2007), Monsoon convection in the Himalayan region as seen by the TRMM Precipitation Radar. Q.J.R. Meteorol. Soc., 133: 1389-1411. doi:10.1002/qj.106 . (TRMM, ヒマラヤ, 降水特性)

• Hunt, K M.R., Turner, A. G. & Schiemann, R K.H.(2022) Katabatic and convective processes drive two preferred peaks in the precipitation diurnal cycle over the Central Himalaya. Q J R Meteorol Soc, 148( 745), 1731– 1751. Available from: https://doi.org/10.1002/qj.4275 (ヒマラヤ・日変化・BSISO・LPS・IMERG）

• Medina, S. , Houze, R. A., Kumar, A. and Niyogi, D. (2010), Summer monsoon convection in the Himalayan region: terrain and land cover effects. Q.J.R. Meteorol. Soc., 136: 593-616. doi:10.1002/qj.601 . (降水特性・TRMM・WRF)

• Ohsawa, T., Ueda, H., Hayashi, T., Watanabe, A., & Matsumoto, J. (2001). Diurnal variations of convective activity and rainfall in tropical Asia. Journal of the Meteorological Society of Japan, 79, 333–352. https://doi.org/10.2151/jmsj.79.333 (アジア全般・日変化・静止気象衛星）

• Shrestha, D., Singh, P., and Nakamura, K. ( 2012), Spatiotemporal variation of rainfall over the central Himalayan region revealed by TRMM Precipitation Radar, J. Geophys. Res., 117, D22106, doi:10.1029/2012JD018140. (ヒマラヤ・TRMM-PR・ダブルバンド・地形)

• Tan, J., Huffman, G. J., Bolvin, D. T., & Nelkin, E. J. (2019). Diurnal cycle of IMERG V06 precipitation. Geophysical Research Letters, 46, 13584–13592. https://doi.org/10.1029/2019GL085395（IMERG)

• Terao, T., F. Murata, Y. Yamane, M. Kiguchi, A. Fukushima, M. Tanoue, S. Ahmed, S. A. Choudhury, H. J. Syiemlieh, L. Cajee, A. K. Bhagabati, P. Bhattacharya, S. Dutta, R. Mahanta, and T. Hayashi, 2017: Direct validation of TRMM/PR near surface rain over the northeastern Indian subcontinent using a tipping bucket raingauge network. SOLA, 13, 157−162, doi:10.2151/sola.2017-029. (メガラヤ高原・地点降水量・TRMM-PR・比較)

• Yamamoto M. K., K. Ueno, and K. Nakamura, 2011: Comparison of Satellite Precipitation Products with Rain Gauge Data for the Khumb Region, Nepal Himalayas. J. Meteorol. Soc. Japan,89(6), 597-610. (シャンボチェ・地点降水量・衛星降水量・比較)

降水変動・極端降水

• Bohlinger, P, Sorteberg, A, Liu, C, Rasmussen, R, Sodemann, H, Ogawa, F. (2019): Multiscale characteristics of an extreme precipitation event over Nepal. Q J R Meteorol Soc., 145, 179– 196. https://doi.org/10.1002/qj.3418(亜熱帯ジェット気流上の準定常ロスビー波・ヒマラヤ・豪雨)

• Goswami, B. N., Ajayamohan, R. S., Xavier, P. K., and Sengupta, D. (2003), Clustering of synoptic activity by Indian summer monsoon intraseasonal oscillations, Geophys. Res. Lett., 30, 1431, doi:10.1029/2002GL016734, 8. (BSISO, QBW, LPS)

• Fujinami, H., T. Yasunari and A. Morimoto, 2014: Dynamics of distinct intraseasonal oscillation in summer monsoon rainfall over the Meghalaya-Bangladesh-western Myanmar region：Covariability between the tropics and mid-latitudes, Clim. Dyn. 43, 2147-2166, DOI: 10.1007/s00382-013-2040-1 (季節内振動・ガンジス平原・QBW).

• Fujinami, H., Sato, T., Kanamori, H. & Murata, F. ( 2017). Contrasting features of monsoon precipitation around the meghalaya plateau under westerly and easterly regimes. Journal of Geophysical Research: Atmospheres, 122, 9591– 9610, https://doi.org/10.1002/2016JD026116 (メガラヤ高原・季節内振動・日変化・陸面過程・LLJ・TRMM-PR)

• Fujinami, H. H. Hirata, M. Kato and K. Tsuboki (2020). Mesoscale precipitation systems and their role in the rapid development of a monsoon depression over the Bay of Bengal, Quart. J. Roy. Meteor. Soc., 146, 267- 283, https://doi.org/10.1002/qj.3672 (LPS・MCS)

• Fujinami, H., T. Sato, H. Kanamori, and M. Kato (2022). Nocturnal southerly moist surge parallel to the coastline over the western Bay of Bengal, Geophysical Research Letters. doi: 10.1029/2022GL100174

• Habib, SMA, Sato, T, Hatsuzuka, D. Decreasing number of propagating mesoscale convective systems in Bangladesh and surrounding area during 1998–2015. Atmos Sci Lett. 2019; 20:e879. https://doi.org/10.1002/asl.879 (バングラデシュ・降水システム・長期変化傾向）

• Hatsuzuka, D, T. Yasunari and H. Fujinami, 2014: Characteristics of low pressure systems associated with intraseasonal oscillation of rainfall over Bangladesh during boreal summer, Mon. Wea. Rev., 142, 4758-4774, DOI: 10.1175/MWR-D-13-00307.1 (LPS・QBW）

• Hatsuzuka, D. and H. Fujinami (2017). Effects of the South Asian monsoon intraseasonal modes on genesis of low pressure systems over Bangladesh, J. Climate, 30, 2481-2499 , DOI:10.1175/jcli-d-16-0360.1 (LPS・QBW・BSISO)

• Hirata, H., Fujinami, H., Kanamori, H., Sato, Y., Kayastha R. B., Shrestha, M. L. and K. Fujita (2022). Multiscale processes leading to heavy precipitation in the eastern Nepal Himalayas (submitted to Journal of Hydrometeorology and in revision) (豪雨・地点雨量計・Meteosat・ERA5・雲解像モデル）

• Kikuchi, K., (2021). The Boreal Summer Intraseasonal Oscillation (BSISO): A Review, Journal of the Meteorological Society of Japan. 99, 933-972.

• Murata, F., T. Terao, H. Fujinami, T. Hayashi, H. Asada, J. Matsumoto, Hiambok Jones Syiemlieh ('2017). Dominant synoptic disturbance in the extreme rainfall at Cherrapunji, North East India based on 100 years of rainfall data, J. Climate, 30, 8237-8251, doi:10.1175/JCLI-D-16-0435.1. （Extreme rainfall, Meghalaya)

• Sato, T., 2013: Mechanism of Orographic Precipitation around the Meghalaya Plateau Associated with Intraseasonal Oscillation and the Diurnal Cycle. Mon. Wea. Rev., 141, 2451–2466, https://doi.org/10.1175/MWR-D-12-00321.1 (メガラヤ高原・季節内振動・日変化・WRF)

• Yanase, W., M. Satoh, H. Taniguchi and H. Fujinami, 2012: Seasonal and intra-seasonal modulation of tropical cyclogenesis environment over the Bay of Bengal during the extended summer monsoon, J. Climate, 25, 2914-2930, DOI: 10.1175/JCLI-D-11-00208.1. (Bay of Bengal, BSISO, LPS)

• Yasunari, T. 1976, Spectral analysis of monsoonal precipitation in the Nepal Himalaya,Seppyo, 38, 59-65.

• Yasunari, T. and J. Inoue, 1978: Characteristics of monsoonal precipitation around peaks and ridges in Shorong and Khumbu Himal, Journal of the Japanese Society of Snow and Ice, 40,26-32.

領域モデル(WRF, CReSS):

• Lin, C., Chen, D., Yang, K., & Ou, T. (2018). Impact of model resolution on simulating the water vapor transport through the central Himalayas: Implication for models’ wet bias over the Tibetan Plateau. Climate Dynamics, 51, 3195– 3207.

• Potter, E. R., Orr, A., Willis, I. C., Bannister, D., & Salerno, F. ( 2018). Dynamical drivers of the local wind regime in a Himalayan valley. Journal of Geophysical Research: Atmospheres, 123, 13,186– 13,202. https://doi.org/10.1029/2018JD029427 (クンブヒマラヤ・局地循環・WRF)

• Sugimoto, S., K. Ueno, H. Fujinami, T. Nasuno, T. Sato and H. G. Takahashi, 2021: Cloud-resolving-model simulations of nocturnal precipitation over the Himalayan slopes and foothills, Journal of Hydrometeorology, 22, 3171-3188.

気候システム：

• Boos, W. R. and Z. Kuang, 2010: Dominant control of the South Asian monsoon by orographic insulation versus plateau heating, Nature, 463, 218-222.