請用此 Handle URI 來引用此文件:
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/29969
完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 柯文雄(Wen-Shung Kau),周明達(Ming-Dah Chou) | |
dc.contributor.author | Hui-Wen Chuang | en |
dc.contributor.author | 莊蕙文 | zh_TW |
dc.date.accessioned | 2021-06-13T01:28:01Z | - |
dc.date.available | 2007-07-23 | |
dc.date.copyright | 2007-07-23 | |
dc.date.issued | 2007 | |
dc.date.submitted | 2007-07-13 | |
dc.identifier.citation | Araki, R., M. D. Yamanaka, et al. (2006). 'Seasonal and interannual variations of diur-nal cycles of wind and cloud activity observed at Serpong, West Jawa, Indone-sia.' Journal of the Meteorological Society of Japan 84A: 171-194.
Bergman, J. W. and M. L. Salby (1997). 'The role of cloud diurnal variations in the time-mean energy budget.' Journal of Climate 10(5): 1114-1124. Betts, A. K. and J. H. Ball (1995). 'The FIFE surface diurnal cycle climate.' Journal of Geophysical Research-Atmospheres 100(D12): 25679-25693. Brown, A. R., R. T. Cederwall, et al. (2002). 'Large-eddy simulation of the diurnal cycle of shallow cumulus convection overland.' Quarterly Journal of the Royal Mete-orological Society 128(582): 1075-1093. Chang, A. T. C., L. S. Chiu, et al. (1995). 'Diurnal Cycle of Oceanic Precipitation from Ssm/I Data.' Monthly Weather Review 123(11): 3371-3380. Chang, C. P., P. A. Harr, et al. (2005). 'Synoptic disturbances over the equatorial South China Sea and western Maritime Continent during boreal winter.' Monthly Weather Review 133(3): 489-503. Chen, S. S. and R. A. Houze (1997). 'Diurnal variation and life-cycle of deep convec-tive systems over the Tropical Pacific warm pool.' Quarterly Journal of the Royal Meteorological Society 123(538): 357-388. Chen, Y. L. and A. J. Nash (1994). 'Diurnal-Variation of Surface Air-Flow and Rainfall Frequencies on the Island of Hawaii.' Monthly Weather Review 122(1): 34-56. Dai, A., K. E. Trenberth, et al. (1999). 'Effects of clouds, soil moisture, precipitation, and water vapor on diurnal temperature range.' Journal of Climate 12(8): 2451-2473. Dai, A. G. (2001). 'Global precipitation and thunderstorm frequencies. Part II: Diurnal variations.' Journal of Climate 14(6): 1112-1128. Dai, A. G. and C. Deser (1999). 'Diurnal and semidiurnal variations in global surface wind and divergence fields.' Journal of Geophysical Research-Atmospheres 104(D24): 31109-31125. Dias, P. L. S., J. P. Bonatti, et al. (1987). 'Diurnally Forced Tropical Tropospheric Cir-culation over South-America.' Monthly Weather Review 115(8): 1465-1478. Garland, J. A. and R. G. Derwent (1979). 'Destruction at the Ground and the Diurnal Cycle of Concentration of Ozone and Other Gases.' Quarterly Journal of the Royal Meteorological Society 105(443): 169-183. Garreaud, R. D. and J. M. Wallace (1997). 'The diurnal march of convective cloudiness over the Americas.' Monthly Weather Review 125(12): 3157-3171. Gray, W. M. and R. W. Jacobson (1977). 'Diurnal-Variation of Deep Cumulus Convec-tion.' Monthly Weather Review 105(9): 1171-1188. Halpern, D. and R. K. Reed (1976). 'Heat Budget of Upper Ocean under Light Winds.' Journal of Physical Oceanography 6(6): 972-975. Hansen, J., M. Sato, et al. (1995). 'Long-Term Changes of the Diurnal Temperature Cy-cle - Implications About Mechanisms of Global Climate-Change.' Atmospheric Research 37(1-3): 175-209. Hendon, H. H. and K. Woodberry (1993). 'The Diurnal Cycle of Tropical Convection.' Journal of Geophysical Research-Atmospheres 98(D9): 16623-16637. Hirose, M. and K. Nakamura (2005). 'Spatial and diurnal variation of precipitation sys-tems over Asia observed by the TRMM Precipitation Radar.' Journal of Geo-physical Research-Atmospheres 110(D5). Ichikawa, H. and T. Yasunari (2006). 'Time-space characteristics of diurnal rainfall over Borneo and surrounding oceans as observed by TRMM-PR.' Journal of Climate 19(7): 1238-1260. Jacobi, C., Y. I. Portnyagin, et al. (1999). 'Climatology of the semidiurnal tide at 52-56 degrees N from ground-based radar wind measurements 1985-1995.' Journal of Atmospheric and Solar-Terrestrial Physics 61(13): 975-991. Janowiak, J. E., P. A. Arkin, et al. (1994). 'An Examination of the Diurnal Cycle in Oceanic Tropical Rainfall Using Satellite and in-Situ Data.' Monthly Weather Review 122(10): 2296-2311. Kozu, T., K. K. Reddy, et al. (2006). 'Seasonal and diurnal variations of raindrop size distribution in Asian monsoon region.' Journal of the Meteorological Society of Japan 84A: 195-209. Kraus, E. B. (1963). 'The Diurnal Precipitation Change over the Sea.' Journal of the Atmospheric Sciences 20(6): 551-556. Kunze, E. and J. M. Toole (1997). 'Tidally driven vorticity, diurnal shear, and turbu-lence atop Fieberling Seamount.' Journal of Physical Oceanography 27(12): 2663-2693. Liberti, G. L., F. Cheruy, et al. (2001). 'Land effect on the diurnal cycle of clouds over the TOGA COARE area, as observed from GMS IR data.' Monthly Weather Review 129(6): 1500-1517. Lin, X., D. A. Randall, et al. (2000). 'Diurnal variability of the hydrologic cycle and radiative fluxes: Comparisons between observations and a GCM.' Journal of Climate 13(23): 4159-4179. Mapes, B. E. and R. A. Houze (1993). 'Cloud Clusters and Superclusters over the Oce-anic Warm Pool.' Monthly Weather Review 121(5): 1398-1415. McGarry, M. M. and R. J. Reed (1978). 'Diurnal-Variations in Convective Activity and Precipitation During Phases 2 and 3 of Gate.' Monthly Weather Review 106(1): 101-113. Morcrette, J. J. (1991). 'Evaluation of Model-Generated Cloudiness - Satel-lite-Observed and Model-Generated Diurnal Variability of Brightness Tempera-ture.' Monthly Weather Review 119(5): 1205-1224. Murata, F., M. D. Yamanaka, et al. (2006). 'Dry intrusions following east-ward-propagating synoptic-scale cloud systems over Sumatera Island.' Journal of the Meteorological Society of Japan 84(2): 277-294. Negri, A. J., T. L. Bell, et al. (2002). 'Sampling of the diurnal cycle of precipitation us-ing TRMM.' Journal of Atmospheric and Oceanic Technology 19(9): 1333-1344. Nesbitt, S. W. and E. J. Zipser (2003). 'The diurnal cycle of rainfall and convective in-tensity according to three years of TRMM measurements.' Journal of Climate 16(10): 1456-1475. Nitta, T. and S. Sekine (1994). 'Diurnal-Variation of Convective Activity over the Tropical Western Pacific.' Journal of the Meteorological Society of Japan 72(5): 627-641. Ohsawa, T., H. Ueda, et al. (2001). 'Diurnal variations of connective activity and rain-fall in tropical Asia.' Journal of the Meteorological Society of Japan 79(1B): 333-352. Randall, D. A., Harshvardhan, et al. (1991). 'Diurnal Variability of the Hydro-logic-Cycle in a General-Circulation Model.' Journal of the Atmospheric Sci-ences 48(1): 40-62. Reed, R. J. and K. D. Jaffe (1981). 'Diurnal-Variation of Summer Convection over West-Africa and the Tropical Eastern Atlantic During 1974 and 1978.' Monthly Weather Review 109(12): 2527-2534. Roble, R. G., J. E. Salah, et al. (1977). 'Seasonal-Variation of Diurnal Thermospheric Winds over Millstone Hill During Solar-Cycle Maximum.' Journal of Atmos-pheric and Terrestrial Physics 39(4): 503-511. Rozendaal, M. A., C. B. Leovy, et al. (1995). 'An Observational Study of Diur-nal-Variations of Marine Stratiform Cloud.' Journal of Climate 8(7): 1795-1809. Sakurai, N., F. Murata, et al. (2005). 'Diurnal cycle of cloud system migration over su-matera island.' Journal of the Meteorological Society of Japan 83(5): 835-850. Sato, T. and F. Kimura (2005). 'Diurnal cycle of convective instability around the cen-tral mountains in Japan during the warm season.' Journal of the Atmospheric Sciences 62(5): 1626-1636. States, R. J. and C. S. Gardner (2000). 'Thermal structure of the mesopause region (80-105 km) at 40 degrees N latitude. Part II: Diurnal variations.' Journal of the Atmospheric Sciences 57(1): 78-92. Stramma, L., P. Cornillon, et al. (1986). 'Large Diurnal Sea-Surface Temperature Vari-ability - Satellite and Insitu Measurements.' Journal of Physical Oceanography 16(5): 827-837. Sui, C. H., K. M. Lau, et al. (1997). 'Diurnal variations in tropical oceanic cumulus convection during TOGA COARE.' Journal of the Atmospheric Sciences 54(5): 639-655. Sui, C. H., X. Li, et al. (1998). 'Radiative-convective processes in simulated diurnal variations of tropical oceanic convection.' Journal of the Atmospheric Sciences 55(13): 2345-2357. Takayabu, Y. N., K. M. Lau, et al. (1996). 'Observation of a quasi-2-day wave during TOGA COARE.' Monthly Weather Review 124(9): 1892-1913. Tao, W. K., S. Lang, et al. (1996). 'Mechanisms of cloud-radiation interaction in the tropics and midlatitudes.' Journal of the Atmospheric Sciences 53(18): 2624-2651. Tian, B. J., D. E. Waliser, et al. (2006). 'Modulation of the diurnal cycle of tropical deep convective clouds by the MJO.' Geophysical Research Letters 33(20). Titheridge, J. E. (1993). 'Atmospheric Winds Calculated from Diurnal Changes in the Midlatitude Ionosphere.' Journal of Atmospheric and Terrestrial Physics 55(13): 1637-1659. Webster, P. J., C. A. Clayson, et al. (1996). 'Clouds, radiation, and the diurnal cycle of sea surface temperature in the Tropical Western Pacific.' Journal of Climate 9(8): 1712-1730. Yang, G. Y. and J. Slingo (2001). 'The diurnal cycle in the Tropics.' Monthly Weather Review 129(4): 784-801. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/29969 | - |
dc.description.abstract | 本研究利用日本氣象衛星(GMS-5)所提供之高解析度的亮度溫度(Tbb)資料來探討1997-2003年冬季在海洋大陸地區雲的日夜變化。利用25小時滑動平均的方法,將原始資料分成兩種時間尺度:一天內時間尺度(日夜變化)、大於一天以上時間尺度。結果顯示,在大的島嶼地區,雲的擾動主要是由於日夜變化的影響,而受到一天以上時間尺度的影響較小;在海洋地區,情況相反,日夜變化對於雲振盪的影響較小,一天以上時間尺度的振盪對於雲振盪的貢獻較大。區域性的熱力影響是造成島嶼上方雲振盪的主因,大尺度的大氣擾動則是對海洋上方的雲變化有較大的影響。
結果也顯示,雲日夜變化的振幅在對流活躍時期會增強;但是,日夜變化的相位則與島嶼或海洋上的大尺度對流的強度無關,而只和區域性的熱力過程有關。在對流活躍時期,海洋上雲日夜變化振幅的增強效果比島嶼的來的明顯。 陸地上的雲的日夜變化主要和太陽加熱低層熱力直接作用有關;在海洋上則可約略分離出三種型態:在對流海域區域,太陽直接熱力過程造成午後雲的生成;在非對流海域,輻射冷卻的效應使得最高/最多的雲發生在晚上;在鄰近島域的海面地區,雲的日夜變化主要受到鄰近大島嶼的影響,從陸地發展的雲系有向外傳播的現象,在海洋大陸相位傳播的速度約5-10m/s,此現象可傳播到距島嶼幾百公里遠的海面上。 | zh_TW |
dc.description.abstract | The high resolution (hourly, resampled to 0.50×0.50) window (11.5μm~12.5μm ) brightness temperature (Tbb) data from Japan’s Geostationary Meteorological Satellite-5 (GMS-5) during 1997-2003 were used to investigate the diurnal variation of clouds in the Maritime Continent during boreal winter. The results showed that a low value of the mean Tbb accompanied a high value of the Tbb standard deviation in the Maritime Con-tinent during boreal winter. Over large islands, the total variance of cloud fluctuation was primarily contributed from the diurnal variation with only a minor contribution from the variations with a time scale longer than one day. Over the oceans, on the other hand, the diurnal variation had an insignificant contribution to the total variance of cloud fluctuations. We can conclude that the local thermodynamic effect is the domi-nating factor causing cloud variations over island. The large scale atmospheric distur-bances have a large impact on cloud variations over oceans but not over islands.
The results also showed that the diurnal variation of clouds is enhanced during the active phase periods, and the diurnal phase is only related to the local dynamic process but not related to the intensity of large-scale convection over both islands and oceans. During the active phase, the diurnal amplitude is much amplified over oceans than that over lands. The diurnal variation of clouds over the land region is mainly due to local thermo-dynamic response to the solar heating cycle. Over the oceans, three types of mecha-nisms could be separated. Over the convective ocean, it could be suggested that ther-modynamic response contributes to the maximum cloudiness in the afternoon. Over non-convective oceans, the radiation cooling could be the reason for the maximum cloudiness during night time. Over the oceans adjacent to lands, the diurnal variation of clouds is highly influenced by land effect resulting in a phase propagating to several hundred kilometers oceans from lands. | en |
dc.description.provenance | Made available in DSpace on 2021-06-13T01:28:01Z (GMT). No. of bitstreams: 1 ntu-96-R94229001-1.pdf: 5835390 bytes, checksum: c9703646605e7256745e88d2f73b8282 (MD5) Previous issue date: 2007 | en |
dc.description.tableofcontents | List of Figures V
List of Tables X Chapter 1. Introduction 1 Chapter 2. Data and Methods 5 Chapter 3. Results 8 3.1 General features 8 3.2 Cloud variations during boreal winter 9 3.3 Diurnal variations 10 3.3.1 Borneo and New Guinea 10 3.3.2 Oceanic regions 11 3.4 Tbb with wind field pattern 12 3.5 Active and inactive phases 13 3.5.1 Borneo and New Guinea 13 3.5.2 Oceanic regions 14 Chapter 4. Discussion 16 4.1 Over lands 16 4.2 Over oceans 17 4.2.1 Non-convective oceanic regions 17 4.2.2 Convective oceanic regions 17 4.2.3 Oceanic regions adjacent to island 18 4.3 Active phase and inactive phase 19 Chapter 5. Summary 21 Appendix- 1998-2002 JJA 23 References 25 | |
dc.language.iso | en | |
dc.title | 雲在海洋大陸的日夜變化 | zh_TW |
dc.title | Diurnal Variation of Clouds over the Maritime Continent | en |
dc.type | Thesis | |
dc.date.schoolyear | 95-2 | |
dc.description.degree | 碩士 | |
dc.contributor.advisor-orcid | ,周明達(mdchou@atmos1.as.ntu.edu.tw) | |
dc.contributor.oralexamcommittee | 許晃雄(Huang-Hsung Hsu),陳正達,周佳(Chia Chou) | |
dc.subject.keyword | 日夜變化,亮度溫度,雲,海洋大陸,振幅,相位, | zh_TW |
dc.subject.keyword | diurnal variation,brightness temperature,cloud,maritime continent,amplitude,phase, | en |
dc.relation.page | 64 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2007-07-17 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 大氣科學研究所 | zh_TW |
顯示於系所單位: | 大氣科學系 |
文件中的檔案:
檔案 | 大小 | 格式 | |
---|---|---|---|
ntu-96-1.pdf 目前未授權公開取用 | 5.7 MB | Adobe PDF |
系統中的文件,除了特別指名其著作權條款之外,均受到著作權保護,並且保留所有的權利。