391 results on '"Chang, C.P."'
Search Results
152. MOSFET's with one-mask sealed diffusion-junctions for ULSI applications
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Liu, C.T., primary, Chang, C.P., additional, Lee, K.H., additional, and Liu, R., additional
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- 1995
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153. Electroabsorption of thin AlAs/GaAs quantum well: Effect of Γ-X valley mixing
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Chang, C.P., primary and Lu, Yan-Ten, additional
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- 1994
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154. Ligand-induced internalization of the epidermal growth factor receptor is mediated by multiple endocytic codes analogous to the tyrosine motif found in constitutively internalized receptors.
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Chang, C.P., primary, Lazar, C.S., additional, Walsh, B.J., additional, Komuro, M, additional, Collawn, J.F., additional, Kuhn, L.A., additional, Tainer, J.A., additional, Trowbridge, I.S., additional, Farquhar, M.G., additional, and Rosenfeld, M.G., additional
- Published
- 1993
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155. Stress-strain behavior of fine-grained alloys
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Wang, S.H., primary, Kao, P.W., additional, and Chang, C.P., additional
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- 1993
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156. Aluminum Electrodeposition from Room Temperature Molten AlCl3-BPC Salt Bath
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Yang, C.C., primary and Chang, C.P., additional
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- 1993
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157. Contribution of platelet microparticle formation and granule secretion to the transmembrane migration of phosphatidylserine.
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Chang, C.P., primary, Zhao, J., additional, Wiedmer, T., additional, and Sims, P.J., additional
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- 1993
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158. Microstructural development in AlSiC composites made by resistance sintering of mechanically alloyed powders
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Hong, S.J., primary, Kao, P.W., additional, and Chang, C.P., additional
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- 1992
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159. A highly manufacturable corner rounding solution for 0.18 /spl mu/m shallow trench isolation.
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Chang, C.P., Pai, C.S., Baumann, F.H., Liu, C.T., Rafferty, C.S., Pinto, M.R., Lloyd, E.J., Bude, M., Klemens, F.P., Miner, J.F., Cheung, K.P., Colonell, J.I., Lai, W.Y.C., Vaidya, H., Hillenius, S.J., Liu, R.C., and Clemens, J.T.
- Published
- 1997
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160. Impact of plasma-charging damage polarity on MOSFET noise.
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Cheung, K.P., Martin, S., Misra, D., Steiner, K., Colonell, J.I., Chang, C.P., Lai, W.Y.C., Liu, C.T., Liu, R., and Pai, C.S.
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- 1997
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161. Intrinsic and stress-induced traps in the direct tunneling current of 2.3-3.8 nm oxides and unified characterization methodologies of sub-3 nm oxides.
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Liu, C.T., Ghetti, A., Ma, Y., Alers, G., Chang, C.P., Cheung, K.P., Colonell, J.I., Lai, W.Y.C., Pai, C.S., Liu, R., Vaidya, H., and Clemens, J.T.
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- 1997
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162. Multiple gate oxide thickness for 2 GHz system-on-a-chip technologies.
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Liu, C.T., Ma, Y., Oh, M., Diodato, P.W., Stiles, K.R., Mcmacken, J.R., Li, F., Chang, C.P., Cheung, K.P., Colonell, J.I., Lai, W.Y.C., Liu, R., Lloyd, E.J., Miner, J.F., Pai, C.S., Vaidya, H., Frackoviak, J., Timko, A., Klemens, F., and Maynard, H.
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- 1998
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163. High-performance CMOS with oxidation-planarized twin tubs and one-mask sealed diffusion-junctions.
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Liu, C.T., Luftman, H., Lin, W., Chang, C.P., Yang, T.S., Fu, C.C., Lee, K.H., Liu, R., and Yaney, D.S.
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- 1993
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164. Ligand-induced internalization and increased cell calcium are mediated via distinct structural elements in the carboxyl terminus of the epidermal growth factor receptor.
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Chang, C.P., primary, Kao, J.P., additional, Lazar, C.S., additional, Walsh, B.J., additional, Wells, A., additional, Wiley, H.S., additional, Gill, G.N., additional, and Rosenfeld, M.G., additional
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- 1991
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165. Aspects of erosional wear behavior during tumbling of BaTiO3 dielectric ceramics
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Chen, S.K., primary, Chang, C.P., additional, and Liu, H.S., additional
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- 1991
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166. Differential diagnosis of tumor-like appearance of the papilla of Vater
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Chang, C.P., primary, Ng, W.W., additional, Tsay, S.H., additional, Lai, K.H., additional, and Lee, S.D., additional
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- 1990
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167. A Theory for the Indian Ocean Dipole–Zonal Mode.
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Tim Li, Bin Wang, Chang, C.P., and Yongsheng Zhang
- Subjects
OCEAN waves ,ATMOSPHERE - Abstract
Four fundamental differences of air–sea interactions between the tropical Pacific and Indian Oceans are identified based on observational analyses and physical reasoning. The first difference is represented by the strong contrast of a zonal cloud–SST phase relationship between the warm and cool oceans. The in-phase cloud–SST relationship in the warm oceans leads to a strong negative feedback, while a significant phase difference in the cold tongue leads to a much weaker thermodynamic damping. The second difference arises from the reversal of the basic-state zonal wind and the tilting of the ocean thermocline, which leads to distinctive effects of ocean waves. The third difference lies in the existence of the Asian monsoon and its interaction with the adjacent oceans. The fourth difference is that the southeast Indian Ocean is a region where a positive atmosphere–ocean thermodynamic feedback exists in boreal summer. A conceptual coupled atmosphere–ocean model was constructed aimed to understand the origin of the Indian Ocean dipole–zonal mode (IODM). In the model, various positive and negative air–sea feedback processes were considered. Among them were the cloud–radiation–SST feedback, the evaporation–SST–wind feedback, the thermocline–SST feedback, and the monsoon–ocean feedback. Numerical results indicate that the IODM is a dynamically coupled atmosphere–ocean mode whose instability depends on the annual cycle of the basic state. It tends to develop rapidly in boreal summer but decay in boreal winter. As a result, the IODM has a distinctive evolution characteristic compared to the El Niño. Sensitivity experiments suggest that the IODM is a weakly damped oscillator in the absence of external forcing, owing to a strong negative cloud–SST feedback and a deep mean thermocline in the equatorial Indian Ocean. A thermodynamic air–sea (TAS) feedback arises from the interaction between an anomalous atmospheric anticyclone and a cold SST anomaly (SSTA) off Sumatra. Because of its dependence on the basic-state wind, the nature of this TAS feedback is season dependent. A positive feedback occurs only in northern summer when the southeasterly flow is pronounced. It becomes a negative feedback in northern winter when the northwesterly wind is pronounced. The phase locking of the IODM can be, to a large extent, explained by this seasonal-dependent TAS feedback. The biennial tendency of the IODM is attributed to the monsoon–ocean feedback and the remote El Niño forcing that has a quasi-biennial component. In the presence of realistic Niño-3 SSTA forcing, the model is capable of simulating IODM events during the last 50 yr that are associated with the El Niño, indicating that ENSO is one of triggering mechanisms. The failure of simulation of the 1961 and 1994 events suggests that other types of climate forcings in addition to the ENSO must play a role in triggering an IODM event. [ABSTRACT FROM AUTHOR]
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- 2003
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168. Magnetoband structures of <f>AB</f>-stacked zigzag nanographite ribbons
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Chang, C.P., Chiu, C.W., Shyu, F.L., Chen, R.B., and Lin, M.F.
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ENERGY level densities , *LANDAU levels - Abstract
Magnetoband structures of
AB -stacked zigzag nanographite ribbons are studied by the tight-binding model. The magnetic field changes band width, energy space, and energy dispersions (the produce of Landau subbands and Landau levels). It causes many zero energy points. Such points and corresponding localized states are studied in detail. There are certain important differences between localized states and edge states. Oscillation period of Landau subbands are determined by these points. The interribbon interactions also affect magnetoband structures, such as energy dispersions, band width, oscillation period of Landau subbands, and flux dependence of Hofstadter butterflies. [Copyright &y& Elsevier]- Published
- 2002
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169. Structural evolution and significance of a m é lange in a collision belt: the Lichi M é lange and the Taiwan arc-continent collision.
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Chang, C.P., Angelier, J., Huang, C.Y., and Liu, C.S.
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MELANGES (Petrology) , *GEOLOGY - Abstract
Presents a study that examined the nature, origin and significance of a meacutelange in a collision belt. Description of the Lichi Meacutelange; Geological maps and structural profiles in the Lichi Meacutelange; Discussion on stratigraphic relationships between the meacutelange and its adjacent flysch formation; Inferences from observations on the Lichi Meacutelange and the Huatung Ridge off Southeastern Taiwan.
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- 2001
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170. Comments: telecom leaders from around the world reveal their plans for the future
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Yamaguchi, Haruo, Chang, C.P., Khim, Wong Hung, Crew, Greg, Troughton, Peter, and Abdubrachman, S.
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Telecommunications services industry ,International communications ,Market trend/market analysis ,Future of computing ,Preview of coming year ,International communication -- Forecasts and trends ,Telecommunications services industry -- Forecasts and trends ,Communications industry -- Forecasts and trends ,Technological forecasting -- Forecasts and trends ,Indonesia -- Science and technology policy ,Hong Kong -- Science and technology policy ,Japan -- Science and technology policy ,Taiwan -- Science and technology policy ,New Zealand -- Science and technology policy ,Singapore -- Science and technology policy - Abstract
Far East & Pacific Japan In 1989, NTT will continue to work to offer new services that match users' needs. Take ISDN, for example. Our major developemtn in this area […]
- Published
- 1989
171. Rapid Thermal Oxide passivation using IC-grade processing.
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Borden, Peter, Li Xu, McDougall, Brendan, Chang, C.P., and Tam, Norman
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- 2008
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172. Search for a Higgs boson decaying into γ⁎γ→ℓℓγ with low dilepton mass in pp collisions at s=8 TeV
- Author
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Khachatryan, V., Sirunyan, A.M., Tumasyan, A., Adam, W., Asilar, E., Bergauer, T., Brandstetter, J., Brondolin, E., Dragicevic, M., Erö, J., Flechl, M., Friedl, M., Frühwirth, R., Ghete, V.M., Hartl, C., Hörmann, N., Hrubec, J., Jeitler, M., Knünz, V., König, A., Krammer, M., Krätschmer, I., Liko, D., Matsushita, T., Mikulec, I., Rabady, D., Rahbaran, B., Rohringer, H., Schieck, J., Schöfbeck, R., Strauss, J., Treberer-Treberspurg, W., Waltenberger, W., Wulz, C.-E., Mossolov, V., Shumeiko, N., Suarez Gonzalez, J., Alderweireldt, S., Cornelis, T., De Wolf, E.A., Janssen, X., Knutsson, A., Lauwers, J., Luyckx, S., Ochesanu, S., Rougny, R., Van De Klundert, M., Van Haevermaet, H., Van Mechelen, P., Van Remortel, N., Van Spilbeeck, A., Abu Zeid, S., Blekman, F., D'Hondt, J., Daci, N., De Bruyn, I., Deroover, K., Heracleous, N., Keaveney, J., Lowette, S., Moreels, L., Olbrechts, A., Python, Q., Strom, D., Tavernier, S., Van Doninck, W., Van Mulders, P., Van Onsem, G.P., Van Parijs, I., Barria, P., Caillol, C., Clerbaux, B., De Lentdecker, G., Delannoy, H., Dobur, D., Fasanella, G., Favart, L., Gay, A.P.R., Grebenyuk, A., Lenzi, T., Léonard, A., Maerschalk, T., Marinov, A., Perniè, L., Randle-conde, A., Reis, T., Seva, T., Vander Velde, C., Vanlaer, P., Yonamine, R., Zenoni, F., Zhang, F., Beernaert, K., Benucci, L., Cimmino, A., Crucy, S., Fagot, A., Garcia, G., Gul, M., Mccartin, J., Ocampo Rios, A.A., Poyraz, D., Ryckbosch, D., Salva, S., Sigamani, M., Strobbe, N., Tytgat, M., Van Driessche, W., Yazgan, E., Zaganidis, N., Basegmez, S., Beluffi, C., Bondu, O., Brochet, S., Bruno, G., Castello, R., Caudron, A., Ceard, L., Da Silveira, G.G., Delaere, C., Favart, D., Forthomme, L., Giammanco, A., Hollar, J., Jafari, A., Jez, P., Komm, M., Lemaitre, V., Mertens, A., Nuttens, C., Perrini, L., Pin, A., Piotrzkowski, K., Popov, A., Quertenmont, L., Selvaggi, M., Vidal Marono, M., Beliy, N., Hammad, G.H., Aldá Júnior, W.L., Alves, G.A., Brito, L., Correa Martins Junior, M., Dos Reis Martins, T., Hensel, C., Mora Herrera, C., Moraes, A., Pol, M.E., Rebello Teles, P., Belchior Batista Das Chagas, E., Carvalho, W., Chinellato, J., Custódio, A., Da Costa, E.M., De Jesus Damiao, D., De Oliveira Martins, C., Fonseca De Souza, S., Huertas Guativa, L.M., Malbouisson, H., Matos Figueiredo, D., Mundim, L., Nogima, H., Prado Da Silva, W.L., Santoro, A., Sznajder, A., Tonelli Manganote, E.J., Vilela Pereira, A., Ahuja, S., Bernardes, C.A., De Souza Santos, A., Dogra, S., Fernandez Perez Tomei, T.R., Gregores, E.M., Mercadante, P.G., Moon, C.S., Novaes, S.F., Padula, Sandra S., Romero Abad, D., Ruiz Vargas, J.C., Aleksandrov, A., Genchev, V., Hadjiiska, R., Iaydjiev, P., Piperov, S., Rodozov, M., Stoykova, S., Sultanov, G., Vutova, M., Dimitrov, A., Glushkov, I., Litov, L., Pavlov, B., Petkov, P., Ahmad, M., Bian, J.G., Chen, G.M., Chen, H.S., Chen, M., Cheng, T., Du, R., Jiang, C.H., Plestina, R., Romeo, F., Shaheen, S.M., Tao, J., Wang, C., Wang, Z., Zhang, H., Asawatangtrakuldee, C., Ban, Y., Li, Q., Liu, S., Mao, Y., Qian, S.J., Wang, D., Xu, Z., Zou, W., Avila, C., Cabrera, A., Chaparro Sierra, L.F., Florez, C., Gomez, J.P., Gomez Moreno, B., Sanabria, J.C., Godinovic, N., Lelas, D., Polic, D., Puljak, I., Antunovic, Z., Kovac, M., Brigljevic, V., Kadija, K., Luetic, J., Micanovic, S., Sudic, L., Attikis, A., Mavromanolakis, G., Mousa, J., Nicolaou, C., Ptochos, F., Razis, P.A., Rykaczewski, H., Bodlak, M., Finger, M., Aly, R., Aly, S., El-khateeb, E., Lotfy, A., Mohamed, A., Radi, A., Salama, E., Sayed, A., Calpas, B., Kadastik, M., Murumaa, M., Raidal, M., Tiko, A., Veelken, C., Eerola, P., Pekkanen, J., Voutilainen, M., Härkönen, J., Karimäki, V., Kinnunen, R., Lampén, T., Lassila-Perini, K., Lehti, S., Lindén, T., Luukka, P., Mäenpää, T., Peltola, T., Tuominen, E., Tuominiemi, J., Tuovinen, E., Wendland, L., Talvitie, J., Tuuva, T., Besancon, M., Couderc, F., Dejardin, M., Denegri, D., Fabbro, B., Faure, J.L., Favaro, C., Ferri, F., Ganjour, S., Givernaud, A., Gras, P., Hamel de Monchenault, G., Jarry, P., Locci, E., Machet, M., Malcles, J., Rander, J., Rosowsky, A., Titov, M., Zghiche, A., Antropov, I., Baffioni, S., Beaudette, F., Busson, P., Cadamuro, L., Chapon, E., Charlot, C., Dahms, T., Davignon, O., Filipovic, N., Florent, A., Granier de Cassagnac, R., Lisniak, S., Mastrolorenzo, L., Miné, P., Naranjo, I.N., Nguyen, M., Ochando, C., Ortona, G., Paganini, P., Regnard, S., Salerno, R., Sauvan, J.B., Sirois, Y., Strebler, T., Yilmaz, Y., Zabi, A., Agram, J.-L., Andrea, J., Aubin, A., Bloch, D., Brom, J.-M., Buttignol, M., Chabert, E.C., Chanon, N., Collard, C., Conte, E., Coubez, X., Fontaine, J.-C., Gelé, D., Goerlach, U., Goetzmann, C., Le Bihan, A.-C., Merlin, J.A., Skovpen, K., Van Hove, P., Gadrat, S., Beauceron, S., Bernet, C., Boudoul, G., Bouvier, E., Carrillo Montoya, C.A., Chasserat, J., Chierici, R., Contardo, D., Courbon, B., Depasse, P., El Mamouni, H., Fan, J., Fay, J., Gascon, S., Gouzevitch, M., Ille, B., Laktineh, I.B., Lethuillier, M., Mirabito, L., Pequegnot, A.L., Perries, S., Ruiz Alvarez, J.D., Sabes, D., Sgandurra, L., Sordini, V., Vander Donckt, M., Verdier, P., Viret, S., Xiao, H., Toriashvili, T., Tsamalaidze, Z., Autermann, C., Beranek, S., Edelhoff, M., Feld, L., Heister, A., Kiesel, M.K., Klein, K., Lipinski, M., Ostapchuk, A., Preuten, M., Raupach, F., Sammet, J., Schael, S., Schulte, J.F., Verlage, T., Weber, H., Wittmer, B., Zhukov, V., Ata, M., Brodski, M., Dietz-Laursonn, E., Duchardt, D., Endres, M., Erdmann, M., Erdweg, S., Esch, T., Fischer, R., Güth, A., Hebbeker, T., Heidemann, C., Hoepfner, K., Klingebiel, D., Knutzen, S., Kreuzer, P., Merschmeyer, M., Meyer, A., Millet, P., Olschewski, M., Padeken, K., Papacz, P., Pook, T., Radziej, M., Reithler, H., Rieger, M., Scheuch, F., Sonnenschein, L., Teyssier, D., Thüer, S., Cherepanov, V., Erdogan, Y., Flügge, G., Geenen, H., Geisler, M., Hoehle, F., Kargoll, B., Kress, T., Kuessel, Y., Künsken, A., Lingemann, J., Nehrkorn, A., Nowack, A., Nugent, I.M., Pistone, C., Pooth, O., Stahl, A., Aldaya Martin, M., Asin, I., Bartosik, N., Behnke, O., Behrens, U., Bell, A.J., Borras, K., Burgmeier, A., Cakir, A., Calligaris, L., Campbell, A., Choudhury, S., Costanza, F., Diez Pardos, C., Dolinska, G., Dooling, S., Dorland, T., Eckerlin, G., Eckstein, D., Eichhorn, T., Flucke, G., Gallo, E., Garay Garcia, J., Geiser, A., Gizhko, A., Gunnellini, P., Hauk, J., Hempel, M., Jung, H., Kalogeropoulos, A., Karacheban, O., Kasemann, M., Katsas, P., Kieseler, J., Kleinwort, C., Korol, I., Lange, W., Leonard, J., Lipka, K., Lobanov, A., Lohmann, W., Mankel, R., Marfin, I., Melzer-Pellmann, I.-A., Meyer, A.B., Mittag, G., Mnich, J., Mussgiller, A., Naumann-Emme, S., Nayak, A., Ntomari, E., Perrey, H., Pitzl, D., Placakyte, R., Raspereza, A., Ribeiro Cipriano, P.M., Roland, B., Sahin, M.Ö., Saxena, P., Schoerner-Sadenius, T., Schröder, M., Seitz, C., Spannagel, S., Trippkewitz, K.D., Wissing, C., Blobel, V., Centis Vignali, M., Draeger, A.R., Erfle, J., Garutti, E., Goebel, K., Gonzalez, D., Görner, M., Haller, J., Hoffmann, M., Höing, R.S., Junkes, A., Klanner, R., Kogler, R., Lapsien, T., Lenz, T., Marchesini, I., Marconi, D., Nowatschin, D., Ott, J., Pantaleo, F., Peiffer, T., Perieanu, A., Pietsch, N., Poehlsen, J., Rathjens, D., Sander, C., Schettler, H., Schleper, P., Schlieckau, E., Schmidt, A., Schwandt, J., Seidel, M., Sola, V., Stadie, H., Steinbrück, G., Tholen, H., Troendle, D., Usai, E., Vanelderen, L., Vanhoefer, A., Akbiyik, M., Barth, C., Baus, C., Berger, J., Böser, C., Butz, E., Chwalek, T., Colombo, F., De Boer, W., Descroix, A., Dierlamm, A., Feindt, M., Frensch, F., Giffels, M., Gilbert, A., Hartmann, F., Husemann, U., Kassel, F., Katkov, I., Kornmayer, A., Lobelle Pardo, P., Mozer, M.U., Müller, T., Müller, Th., Plagge, M., Quast, G., Rabbertz, K., Röcker, S., Roscher, F., Simonis, H.J., Stober, F.M., Ulrich, R., Wagner-Kuhr, J., Wayand, S., Weiler, T., Wöhrmann, C., Wolf, R., Anagnostou, G., Daskalakis, G., Geralis, T., Giakoumopoulou, V.A., Kyriakis, A., Loukas, D., Psallidas, A., Topsis-Giotis, I., Agapitos, A., Kesisoglou, S., Panagiotou, A., Saoulidou, N., Tziaferi, E., Evangelou, I., Flouris, G., Foudas, C., Kokkas, P., Loukas, N., Manthos, N., Papadopoulos, I., Paradas, E., Strologas, J., Bencze, G., Hajdu, C., Hazi, A., Hidas, P., Horvath, D., Sikler, F., Veszpremi, V., Vesztergombi, G., Zsigmond, A.J., Beni, N., Czellar, S., Karancsi, J., Molnar, J., Szillasi, Z., Bartók, M., Makovec, A., Raics, P., Trocsanyi, Z.L., Ujvari, B., Mal, P., Mandal, K., Sahoo, N., Swain, S.K., Bansal, S., Beri, S.B., Bhatnagar, V., Chawla, R., Gupta, R., Bhawandeep, U., Kalsi, A.K., Kaur, A., Kaur, M., Kumar, R., Mehta, A., Mittal, M., Nishu, N., Singh, J.B., Walia, G., Kumar, Ashok, Kumar, Arun, Bhardwaj, A., Choudhary, B.C., Garg, R.B., Kumar, A., Malhotra, S., Naimuddin, M., Ranjan, K., Sharma, R., Sharma, V., Banerjee, S., Bhattacharya, S., Chatterjee, K., Dey, S., Dutta, S., Jain, Sa., Jain, Sh., Khurana, R., Majumdar, N., Modak, A., Mondal, K., Mukherjee, S., Mukhopadhyay, S., Roy, A., Roy, D., Roy Chowdhury, S., Sarkar, S., Sharan, M., Abdulsalam, A., Chudasama, R., Dutta, D., Jha, V., Kumar, V., Mohanty, A.K., Pant, L.M., Shukla, P., Topkar, A., Aziz, T., Bhowmik, S., Chatterjee, R.M., Dewanjee, R.K., Dugad, S., Ganguly, S., Ghosh, S., Guchait, M., Gurtu, A., Kole, G., Kumar, S., Mahakud, B., Maity, M., Majumder, G., Mazumdar, K., Mitra, S., Mohanty, G.B., Parida, B., Sarkar, T., Sudhakar, K., Sur, N., Sutar, B., Wickramage, N., Sharma, S., Bakhshiansohi, H., Behnamian, H., Etesami, S.M., Fahim, A., Goldouzian, R., Khakzad, M., Mohammadi Najafabadi, M., Naseri, M., Paktinat Mehdiabadi, S., Rezaei Hosseinabadi, F., Safarzadeh, B., Zeinali, M., Felcini, M., Grunewald, M., Abbrescia, M., Calabria, C., Caputo, C., Chhibra, S.S., Colaleo, A., Creanza, D., Cristella, L., De Filippis, N., De Palma, M., Fiore, L., Iaselli, G., Maggi, G., Maggi, M., Miniello, G., My, S., Nuzzo, S., Pompili, A., Pugliese, G., Radogna, R., Ranieri, A., Selvaggi, G., Silvestris, L., Venditti, R., Verwilligen, P., Abbiendi, G., Battilana, C., Benvenuti, A.C., Bonacorsi, D., Braibant-Giacomelli, S., Brigliadori, L., Campanini, R., Capiluppi, P., Castro, A., Cavallo, F.R., Codispoti, G., Cuffiani, M., Dallavalle, G.M., Fabbri, F., Fanfani, A., Fasanella, D., Giacomelli, P., Grandi, C., Guiducci, L., Marcellini, S., Masetti, G., Montanari, A., Navarria, F.L., Perrotta, A., Rossi, A.M., Rovelli, T., Siroli, G.P., Tosi, N., Travaglini, R., Cappello, G., Chiorboli, M., Costa, S., Giordano, F., Potenza, R., Tricomi, A., Tuve, C., Barbagli, G., Ciulli, V., Civinini, C., D'Alessandro, R., Focardi, E., Gonzi, S., Gori, V., Lenzi, P., Meschini, M., Paoletti, S., Sguazzoni, G., Tropiano, A., Viliani, L., Benussi, L., Bianco, S., Piccolo, D., Calvelli, V., Ferro, F., Lo Vetere, M., Monge, M.R., Robutti, E., Tosi, S., Brianza, L., Dinardo, 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Sperka, D., Wang, J., Wang, S., Yelton, J., Hewamanage, S., Linn, S., Markowitz, P., Martinez, G., Rodriguez, J.L., Ackert, A., Adams, J.R., Adams, T., Askew, A., Bochenek, J., Diamond, B., Haas, J., Hagopian, S., Hagopian, V., Johnson, K.F., Khatiwada, A., Prosper, H., Veeraraghavan, V., Weinberg, M., Bhopatkar, V., Hohlmann, M., Kalakhety, H., Mareskas-palcek, D., Roy, T., Yumiceva, F., Adams, M.R., Apanasevich, L., Berry, D., Betts, R.R., Bucinskaite, I., Cavanaugh, R., Evdokimov, O., Gauthier, L., Gerber, C.E., Hofman, D.J., Kurt, P., O'Brien, C., Sandoval Gonzalez, I.D., Silkworth, C., Turner, P., Varelas, N., Wu, Z., Zakaria, M., Bilki, B., Clarida, W., Dilsiz, K., Durgut, S., Gandrajula, R.P., Haytmyradov, M., Khristenko, V., Merlo, J.-P., Mermerkaya, H., Mestvirishvili, A., Moeller, A., Nachtman, J., Ogul, H., Onel, Y., Ozok, F., Penzo, A., Snyder, C., Tan, P., Tiras, E., Wetzel, J., Yi, K., Anderson, I., Barnett, B.A., Blumenfeld, B., Fehling, D., Feng, L., Gritsan, A.V., Maksimovic, P., Martin, C., Nash, K., Osherson, M., Swartz, M., Xiao, M., Xin, Y., Baringer, P., Bean, A., Benelli, G., Bruner, C., Gray, J., Kenny III, R.P., Majumder, D., Malek, M., Murray, M., Noonan, D., Sanders, S., Stringer, R., Wang, Q., Wood, J.S., Chakaberia, I., Ivanov, A., Kaadze, K., Khalil, S., Makouski, M., Maravin, Y., Mohammadi, A., Saini, L.K., Skhirtladze, N., Svintradze, I., Toda, S., Lange, D., Rebassoo, F., Wright, D., Anelli, C., Baden, A., Baron, O., Belloni, A., Calvert, B., Eno, S.C., Ferraioli, C., Gomez, J.A., Hadley, N.J., Jabeen, S., Kellogg, R.G., Kolberg, T., Kunkle, J., Lu, Y., Mignerey, A.C., Pedro, K., Shin, Y.H., Skuja, A., Tonjes, M.B., Tonwar, S.C., Apyan, A., Barbieri, R., Baty, A., Bierwagen, K., Brandt, S., Busza, W., Cali, I.A., Demiragli, Z., Di Matteo, L., Gomez Ceballos, G., Goncharov, M., Gulhan, D., Innocenti, G.M., Klute, M., Kovalskyi, D., Lai, Y.S., Lee, Y.-J., Levin, A., Luckey, P.D., Mcginn, C., Mironov, C., Niu, X., Paus, C., Ralph, D., Roland, C., Roland, G., Salfeld-Nebgen, J., Stephans, G.S.F., Sumorok, K., Varma, M., Velicanu, D., Veverka, J., Wang, T.W., Wyslouch, B., Yang, M., Zhukova, V., Dahmes, B., Finkel, A., Gude, A., Hansen, P., Kalafut, S., Kao, S.C., Klapoetke, K., Kubota, Y., Lesko, Z., Mans, J., Nourbakhsh, S., Ruckstuhl, N., Rusack, R., Tambe, N., Turkewitz, J., Acosta, J.G., Oliveros, S., Avdeeva, E., Bloom, K., Bose, S., Claes, D.R., Dominguez, A., Fangmeier, C., Gonzalez Suarez, R., Kamalieddin, R., Keller, J., Knowlton, D., Kravchenko, I., Lazo-Flores, J., Meier, F., Monroy, J., Ratnikov, F., Siado, J.E., Snow, G.R., Alyari, M., Dolen, J., George, J., Godshalk, A., Iashvili, I., Kaisen, J., Kharchilava, A., Rappoccio, S., Alverson, G., Barberis, E., Baumgartel, D., Chasco, M., Hortiangtham, A., Massironi, A., Morse, D.M., Nash, D., Orimoto, T., Teixeira De Lima, R., Trocino, D., Wang, R.-J., Wood, D., Zhang, J., Hahn, K.A., Kubik, A., Mucia, N., Odell, N., Pollack, B., Pozdnyakov, A., Schmitt, M., Stoynev, S., Sung, K., Trovato, M., Velasco, M., Won, S., Brinkerhoff, A., Dev, N., Hildreth, M., Jessop, C., Karmgard, D.J., Kellams, N., Lannon, K., Lynch, S., Marinelli, N., Meng, F., Mueller, C., Musienko, Y., Pearson, T., Planer, M., Reinsvold, A., Ruchti, R., Smith, G., Valls, N., Wayne, M., Wolf, M., Woodard, A., Antonelli, L., Brinson, J., Bylsma, B., Durkin, L.S., Flowers, S., Hart, A., Hill, C., Hughes, R., Kotov, K., Ling, T.Y., Liu, B., Luo, W., Puigh, D., Rodenburg, M., Winer, B.L., Wulsin, H.W., Driga, O., Elmer, P., Hardenbrook, J., Hebda, P., Koay, S.A., Lujan, P., Marlow, D., Medvedeva, T., Mooney, M., Olsen, J., Palmer, C., Piroué, P., Quan, X., Saka, H., Stickland, D., Tully, C., Werner, J.S., Zuranski, A., Barnes, V.E., Benedetti, D., Bortoletto, D., Gutay, L., Jha, M.K., Jones, M., Jung, K., Kress, M., Miller, D.H., Neumeister, N., Primavera, F., Radburn-Smith, B.C., Shi, X., Shipsey, I., Silvers, D., Sun, J., Svyatkovskiy, A., Wang, F., Xie, W., Xu, L., Zablocki, J., Parashar, N., Stupak, J., Adair, A., Akgun, B., Chen, Z., Ecklund, K.M., Geurts, F.J.M., Guilbaud, M., Li, W., Michlin, B., Northup, M., Padley, B.P., Redjimi, R., Roberts, J., Rorie, J., Tu, Z., Zabel, J., Betchart, B., Bodek, A., de Barbaro, P., Demina, R., Eshaq, Y., Ferbel, T., Galanti, M., Garcia-Bellido, A., Goldenzweig, P., Han, J., Harel, A., Hindrichs, O., Khukhunaishvili, A., Petrillo, G., Verzetti, M., Demortier, L., Arora, S., Barker, A., Chou, J.P., Contreras-Campana, C., Contreras-Campana, E., Duggan, D., Ferencek, D., Gershtein, Y., Gray, R., Halkiadakis, E., Hidas, D., Hughes, E., Kaplan, S., Kunnawalkam Elayavalli, R., Lath, A., Panwalkar, S., Park, M., Salur, S., Schnetzer, S., Sheffield, D., Somalwar, S., Stone, R., Thomas, S., Thomassen, P., Walker, M., Foerster, M., Riley, G., Rose, K., Spanier, S., York, A., Bouhali, O., Castaneda Hernandez, A., Dalchenko, M., De Mattia, M., Delgado, A., Dildick, S., Eusebi, R., Flanagan, W., Gilmore, J., Kamon, T., Krutelyov, V., Montalvo, R., Mueller, R., Osipenkov, I., Pakhotin, Y., Patel, R., Perloff, A., Roe, J., Safonov, A., Tatarinov, A., Ulmer, K.A., Akchurin, N., Cowden, C., Damgov, J., Dragoiu, C., Dudero, P.R., Faulkner, J., Kunori, S., Lamichhane, K., Lee, S.W., Libeiro, T., Undleeb, S., Volobouev, I., Appelt, E., Delannoy, A.G., Greene, S., Gurrola, A., Janjam, R., Johns, W., Maguire, C., Melo, A., Sheldon, P., Snook, B., Tuo, S., Velkovska, J., Xu, Q., Arenton, M.W., Boutle, S., Cox, B., Francis, B., Goodell, J., Hirosky, R., Ledovskoy, A., Li, H., Lin, C., Neu, C., Wolfe, E., Wood, J., Xia, F., Clarke, C., Harr, R., Karchin, P.E., Kottachchi Kankanamge Don, C., Lamichhane, P., Sturdy, J., Belknap, D.A., Carlsmith, D., Cepeda, M., Christian, A., Dasu, S., Dodd, L., Duric, S., Friis, E., Gomber, B., Hall-Wilton, R., Herndon, M., Hervé, A., Klabbers, P., Lanaro, A., Levine, A., Long, K., Loveless, R., Mohapatra, A., Ojalvo, I., Perry, T., Pierro, G.A., Polese, G., Ross, I., Ruggles, T., Sarangi, T., Savin, A., Smith, N., Smith, W.H., Taylor, D., and Woods, N.
- Subjects
Dalitz decay ,CMS ,Higgs boson ,Physics ,High Energy Physics::Phenomenology ,High Energy Physics::Experiment - Abstract
A search is described for a Higgs boson decaying into two photons, one of which has an internal conversion to a muon or an electron pair (ℓℓγ). The analysis is performed using proton–proton collision data recorded with the CMS detector at the LHC at a centre-of-mass energy of 8 TeV, corresponding to an integrated luminosity of 19.7 fb−1. The events selected have an opposite-sign muon or electron pair and a high transverse momentum photon. No excess above background has been found in the three-body invariant mass range 120
- Full Text
- View/download PDF
173. A manufacturable embedded fluorinated SiO/sub 2/ for advanced 0.25 /spl mu/m CMOS VLSI multilevel interconnect applications.
- Author
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Pai, C.S., Velaga, A.N., Lindenberger, W.S., Lai, W.Y.-C., Cheung, K.P., Baumann, F.H., Chang, C.P., Liu, C.T., Liu, R., Diodato, P.W., Colonell, J.I., Vaidya, H., Vitkavage, S.C., Clemens, J.T., and Tsubokura, F.
- Published
- 1998
- Full Text
- View/download PDF
174. Dynamics of teleconnections and Walker circulations forced by equatorial heating
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Lim, H., Chang, C.P., Naval Postgraduate School (U.S.), and Meteorology
- Subjects
Physics::Atmospheric and Oceanic Physics - Abstract
Using a linearized model with constant mean wind on an equatorial β-plane, two types of atmospheric response to steady tropical forcing are studied by an eigenmode analysis. The first type is the less rotationally trapped “barotropic” motions which show some of the characteristics of the teleconnection patterns observed by Bjerknes (1966) and Horel and Wallace (1981). The second type is the more rotationally trapped, warm-core, deep baroclinic motions which resemble the Walker circulations. The analysis reveals several important inadequacies in previous modeling studies and provides a relatively comprehensive explanation of the dynamics of both types of motions. A vertical normal mode consideration shows that the barotropic-type motions are difficult to excite by internal beating. Surface heating, which has been neglected in many previous numerical modeling studies, is found to be important in directly forcing this type of motion. Furthermore, the possible contribution by large equivalent depth internal modes to the teleconnection response was not considered in these studies. A ray tracing approach is used to demonstrate the importance of the rotational trapping effect on the propagation of these deep internal modes. A horizontal normal mode analysis shows that the most prominent responses in all cases are band disturbances of Kelvin and Rossby modes. In addition, in a westerly mean wind with a speed within the range of the Rossby wave phase speed, Rossby mode lee waves are also excited. These lee waves are replaced by Rossby mode evanescent disturbances in other mean winds. For large equivalent depths in westerlies, the band disturbances combine to produce the teleconnection pattern. For all equivalent depths, the Rossby mode is very important in the equatorial zonal wind band response on both the cast and the west sides of the forcing. For small equivalent depths this makes the Rossby mode an important component of both the eastern and the western Walker circulations. Several previous models obtained only the Rossby and Kelvin band solutions due to their use of a long- wave approximation. This approximation distorts the responses, with the most serious distortions occurring in mean westerlies. Although the tropical mean wind is often easterly, it is argued that the westerly mean wind solution is probably more relevant to the Walker circulations due to their observed transient nature and the dynamics of transient forcing. In the westerly mean wind solution the Rossby lee waves east of the forcing substantially reduce the longitudinal extent of the zonal wind band to a value comparable to that observed.
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- 1983
175. A high sensitivity lead-titanate (PbTiO3) pyroelectric thin-film infrared sensor with temperature isolation improvement structure.
- Author
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Jyh-Jier Ho, Fang, Y.K., Wu, K.H., Hsieh, W.T., Chu, C.W., Huang, C.R., Ju, M.S., and Chang, C.P.
- Published
- 1998
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- View/download PDF
176. A composite satellite study of the 1972-73 easterly waves in the tropical western Pacific.
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Chang, C.P., Naval Postgraduate school, Meteorology, Delaney, Dennis Michael, Chang, C.P., Naval Postgraduate school, Meteorology, and Delaney, Dennis Michael
- Abstract
In order to obtain further insight into the structure and properties of easterly waves in the tropical western Pacific, subjectively digitized satellite data for the latter half of the years 1972 and 1973, which possess respectively warm and cold sea-surface temperature anomalies, are analyzed using a compositing technique to obtain composites of percentage convective cloud cover during wave passage. The composites are then compared to composites of temperature, relative humidity and meridional winds. The results, in certain ways, are in agreement with those obtained previously by spectral analysis in the proposed structural tilt of the waves. Significant new results are also obtained. The effects of the local sea-surface temperature influence are most important only for the convective activity organized by the waves. On the other hand, the timemean cloudiness is a factor of the larger-scale sea-surface temperature gradient and the associated Walker circulation. Moreover, the vertical structure of the waves may be a function of the vertical shear, but it is unrelated to convective activity.
- Published
- 1977
177. A numerical simulation of the Mei-Yu front and the associated low-level jet
- Author
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Chang, C.P., Williams, R.T., Naval Postgraduate School (U.S.), Meteorology, Chou, Lang C., Chang, C.P., Williams, R.T., Naval Postgraduate School (U.S.), Meteorology, and Chou, Lang C.
- Abstract
The Mei-Yu front is a quasi-stationary belt of heavy precipitation imbedded in the summer monsoon trough over East Asia. This work used a two dimensional frontogenesis model to study the Mei-Yu front, especially its associated low-level jet (LLJ) which often occurs during intense convection. Several numerical experiments were carried out to simulate the quasi-steady frontal structures in different environments. The results resemble many observed features, such as the stronger temperature and moisture gradients in the midlatitude fronts and the stronger horizontal shear and LLJ in the subtropical fronts. The LLJ is most conspicuous in the subtropical simulation when high humidity and surface fluxes are included. The results further suggest that the LLJ is developed through the Coriolis torque that is exerted by the low-level poleward branch of a "reversed Hadley cell" equatorward of the front. This thermally direct cell is different from the normal cross-frontal secondary circulation. Its development depends on the occurrence of intense convection.
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- 1986
178. A study of interannual and intraannual tropical atmospheric circulations during northern hemisphere summer.
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Chang, C.P., Lau, K.M.W., Naval Postgraduate School (U.S.), Meteorology, McCormick, Earle Leslie, Chang, C.P., Lau, K.M.W., Naval Postgraduate School (U.S.), Meteorology, and McCormick, Earle Leslie
- Abstract
This thesis contains a study of the interannual and intraannual tropical atmospheric circulations for the Northern Hemisphere summer seasons of IQTU, 1975 and 1976 using satellite observations of infrared radiation and albedo in conjunction with parameters available from conventional 200 mb data. The 200 mb flow regimes are contrasted for the three seasons and power spectra and cross-spectral analysis are used to find significant correlations between the parameters from time series generated within a given area and between the areas. These areas were picked for each parameter to represent regions of maxim.um time-averaged values. The anomalously warm sea surface temperatures in 1976 (Bepristis, 1977) occurred in conjunction with major circulation changes paralleling Bjerknes' (1959) hypothesis and the differences in flow regimes between a normal and dry monsoon season are in general agreement with Kanamitsu and Krishnamurti (1978). Significant correlations were found to exist between parameters within the eastern Pacific and western Pacific and also between these two regions . Particularly strong correlations involved the u², v² and IR parameters
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- 1978
179. Upper level barotropic instability in the tropics.
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Williams, Roger T., Chang, C.P., Naval Postgraduate School (U.S.), Meteorology, Hartinger, Ronnie J., Williams, Roger T., Chang, C.P., Naval Postgraduate School (U.S.), Meteorology, and Hartinger, Ronnie J.
- Abstract
The structure of barotropically unstable disturbances in the tropics was examined with a two-level quasi-geostrophic model. The forecast equations were linearized and non-dimensionalized and the most unstable mode was found numerically by use of the initial value technique. The wind profile U(j) = a(j)U(o) sech² (y/L) was used. Simple CISK type heating was introduced to determine its effects on the growth of the waves. The jet wind profile was more unstable with easterly flow than westerly flow when no heating or friction was present. When the jet profile was present only at the upper level, the ratio of the disturbance amplitude at the lower level to the disturbance amplitude at the upper level decreased toward the equator. When the heating rate was not large enough to increase the growth rate, the amplitude ratio remained small As the heating rate becomes larger, the ratio increases to a value larger than 1.
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- 1975
180. Midlatitude tropical interactions during winter
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Unspecified Center, Chang, C.P., Unspecified Center, and Chang, C.P.
- Abstract
Pre-FGGE and FGGE/MONEX data are used to identify short term midlatitude tropical and longitudinal interactions during the winter monsoon. These interactions occur as cold surges, which develop over the East Asian continent and penetrate deep into the tropics with fast gravity wave speed. The observed interactions that occur after a surge include cyclogenesis and enhanced convection in the equatorial region, feedback from equatorial convection to midlatitude circulation systems, tropical east-west (Walker) circulations, and cross-equatorial influence. These interactions are also studied theoretically by analytical solutions of linearized shallow water equations. Response to transient forcing (monsoon surges) are mainly in Rossby and Kelvin modes. When the forcing time scale is short, significant gravity modes are also excited. The responses closely resemble observed winter monsoon flow. Responses to stationary forcing show that deep (barotropic) motions propagate energy away into high latitudes and that shallow (baroclinic) motions are trapped around the equator. It is shown that the barotropic teleconnection-type response to tropical sources found in previous numerical studies was due to the specified vertical wind shear and surface friction.
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- 1985
181. A numerical simulation of the Mei-Yu front and the associated low-level jet
- Author
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Chang, C.P., Williams, R.T., Naval Postgraduate School (U.S.), Meteorology, Chou, Lang C., Chang, C.P., Williams, R.T., Naval Postgraduate School (U.S.), Meteorology, and Chou, Lang C.
- Abstract
The Mei-Yu front is a quasi-stationary belt of heavy precipitation imbedded in the summer monsoon trough over East Asia. This work used a two dimensional frontogenesis model to study the Mei-Yu front, especially its associated low-level jet (LLJ) which often occurs during intense convection. Several numerical experiments were carried out to simulate the quasi-steady frontal structures in different environments. The results resemble many observed features, such as the stronger temperature and moisture gradients in the midlatitude fronts and the stronger horizontal shear and LLJ in the subtropical fronts. The LLJ is most conspicuous in the subtropical simulation when high humidity and surface fluxes are included. The results further suggest that the LLJ is developed through the Coriolis torque that is exerted by the low-level poleward branch of a "reversed Hadley cell" equatorward of the front. This thermally direct cell is different from the normal cross-frontal secondary circulation. Its development depends on the occurrence of intense convection., http://archive.org/details/numericalsimulat00chou, Approved for public release; distribution is unlimited.
182. Intraseasonal oscillations over the tropical western Pacific and eastern Indian Ocean for the northern summers of 1989-1991
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Chang, C.P., Chen, Jeng-Ming, Naval Postgraduate School (U.S.), Cardenas Amores, Jorge A., Chang, C.P., Chen, Jeng-Ming, Naval Postgraduate School (U.S.), and Cardenas Amores, Jorge A.
- Abstract
In this study we used data analyzed by the Navy Operational Global Analysis and Prediction System to study the intraseasonal oscillations other than Madden and Julian oscillation over the tropical western Pacific and eastern Indian ocean. The period of study is May-September of 1989, 1990 and 1991. Multiple-set canonical correlation (MCC), single point correlation and composite analyses were used to determine the structure of the disturbances. The results show that MCC mode#l describes both the seasonal change and a near 20 day oscillation with a zonal half-wavelength around 3000-4000 km. The single point correlation and composites indicate that these oscillations are in gradient wind balance, transporting moisture northward, having upper level divergence over a surface low and a warm-core structure. The seasonal change composite shows a quasi-stationary oscillation with May and June corresponding to the negative phase of MCC mode#l, and August corresponding to the positive phase of MCC mode#l. The near 20 day composite describes a westward propagation of 2.5 - 3' per day, with phase 2 corresponding to the negative phase of MCC mode#l and phase 5 corresponding to the positive phase of MCC mode#1, http://archive.org/details/intraseasonalosc1094542885, Ecuadorian Navy author, Approved for public release; distribution is unlimited.
183. South China Sea warm-core and cold-core eddies detected from the Navy's Master Oceanographic Observation Data Set (MOODS)
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Chu, Peter, Chang, C.P., Physical Oceanography, Tseng, Hsing-Chia, Chu, Peter, Chang, C.P., Physical Oceanography, and Tseng, Hsing-Chia
- Abstract
A South China Sea warm core eddy with sea surface temperatures (SST) higher than 29.5 C, recently reported by Chu and Chang (1995), appears in the central South China Sea (west of Luzon Island) in boreal spring, and strengthens until the onset of the summer monsoon (mid-May), then weakens and disappears at the end of May. Although its size and intensity varies, the warm core eddy releases large moisture and heat fluxes into the atmosphere and in turn affects the monsoon circulation. The transient features and interannual variabilities of the warm core eddy have not yet been studied. In this study we use 189,059 temperature profiles from the U.S. Navy's Master Oceanographic Observation Data Set (MOODS) to investigate the eddy features. We use Optimal Interpolation to create a ten-day interval synoptic data set for 1964-84 on a 0.5 x 1 deg. grid (finer resolution in zonal direction) from the MOODS SST data. Then, we formulate an Emprical Orthogonal Functions (EOF) analysis. The first EOF mode accounts for 35.5% of the variance and is characterized by a field which is similar to the mean field. The second EOF mode accounts for 21.4% of the variance and is characterized by a meso-scale eddy (1l6 - 1l9 E, 16 - 19 N) to the west of Luzon Island. The size of the eddy is around 100,000 km2. The time series of EOF2 behave differently between El Niflo and non-El Niflo years: a warm-core eddy often appears during the non- El Niflo years, and a cold-core eddy usually exists during the El Niflo years. A new scenario of the air sea feedback is proposed for the warm core eddy formation in non-El Nino years and the cold core eddy formation in El Nino years., http://archive.org/details/southchinsewarmc109457592, Republic of China Navy author.
184. A composite satellite study of the 1972-73 easterly waves in the tropical western Pacific.
- Author
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Chang, C.P., Naval Postgraduate school, Meteorology, Delaney, Dennis Michael, Chang, C.P., Naval Postgraduate school, Meteorology, and Delaney, Dennis Michael
- Abstract
In order to obtain further insight into the structure and properties of easterly waves in the tropical western Pacific, subjectively digitized satellite data for the latter half of the years 1972 and 1973, which possess respectively warm and cold sea-surface temperature anomalies, are analyzed using a compositing technique to obtain composites of percentage convective cloud cover during wave passage. The composites are then compared to composites of temperature, relative humidity and meridional winds. The results, in certain ways, are in agreement with those obtained previously by spectral analysis in the proposed structural tilt of the waves. Significant new results are also obtained. The effects of the local sea-surface temperature influence are most important only for the convective activity organized by the waves. On the other hand, the timemean cloudiness is a factor of the larger-scale sea-surface temperature gradient and the associated Walker circulation. Moreover, the vertical structure of the waves may be a function of the vertical shear, but it is unrelated to convective activity., http://archive.org/details/acompositesatell1094518051, Lieutenant, United States Navy, Approved for public release; distribution is unlimited.
185. A study of South Asian monsoon convection and tropical upper easterly jet during northern summer 1991
- Author
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Chang, C.P., Chu, Pete, Nicklin, Michael S., Chang, C.P., Chu, Pete, and Nicklin, Michael S.
- Abstract
This work studies the 1991 northern summer monsoon over India and surrounding areas using Japanese (GMS) and Indian (INSAT) geostationary satellite data, the ECMWF objective re-analysis, and the NMC sea surface temperature analysis. Monthly and weekly mean fields are first used to examine the development of the monsoon over the entire domain and to identify the timing of the onset over India. Latent heat fluxes are shown to be important in the monsoon development process. The relationship between the synoptic variations of a convective index derived from satellite data and the upper tropospheric easterly jet show two possible effects of cumulus convection on the easterly jet. The first is a forcing of the jet maximum near southern India when convection flares up to the north in the monsoon trough. This is believed to be the result of the Coriolis acceleration of the southward outflow of the local Hadley cell. The second is a damping of the upper jet by cumulus momentum transport that occurs at the same location as the jet maximum. This second effect is most clearly shown in regions of strong vertical shear., http://archive.org/details/astudyofsouthasi1094532025, NA, U.S. Navy (U.S.N.) author, Approved for public release; distribution is unlimited.
186. Analysis of the East Asian cold surge using a 15-year Navy data set
- Author
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Chen, Jeng Ming, Chang, C.P., Meteorology and Physcical Oceanography, Jarvis, James R., Chen, Jeng Ming, Chang, C.P., Meteorology and Physcical Oceanography, and Jarvis, James R.
- Abstract
The East Asian winter monsoon cold surge is examined using Navy tropical Global Band Analysis data for January-March of 1975-1988. Multiple-set Canonicle Correlation (MCC) analysis, single-point correlation analysis, and composite analysis are used to determine the the cold surge structure over a broad domain that includes the western Pacific and eastern Indian ocean. The results show that the structure of the cold surge is manifested in MCC modes 1 and 2 of surface V calculated over both the East and South China Seas. Single-point correlation and composite analyses indicate that the surge can be viewed as a single mode over a rather broad region, with an average period of 8 days, that includes simultaneous eastward propagating longwaves across the East China Sea and northwestern Pacific, and equatorward propagating surge waves across the South China Sea. Composite analyses during strong events also reveal cross-equatorial surge influence present at low levels and increases in divergence over the maritime continent at 200 hPa. MCC modes 3 and 4 calculated over a small spatial domain that includes the East China Sea describe 3-day eastward propagating waves with wavelengths on the order of 1500-2000 km. Associated with these shorter waves are modest surge waves that also propagate equatorward across the South China Sea., http://archive.org/details/analysisofeastas1094531564, NA, NA, U.S. Navy (U.S.N.) author.
187. A study of interannual and intraannual tropical atmospheric circulations during northern hemisphere summer.
- Author
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Chang, C.P., Lau, K.M.W., Naval Postgraduate School (U.S.), Meteorology, McCormick, Earle Leslie, Chang, C.P., Lau, K.M.W., Naval Postgraduate School (U.S.), Meteorology, and McCormick, Earle Leslie
- Abstract
This thesis contains a study of the interannual and intraannual tropical atmospheric circulations for the Northern Hemisphere summer seasons of IQTU, 1975 and 1976 using satellite observations of infrared radiation and albedo in conjunction with parameters available from conventional 200 mb data. The 200 mb flow regimes are contrasted for the three seasons and power spectra and cross-spectral analysis are used to find significant correlations between the parameters from time series generated within a given area and between the areas. These areas were picked for each parameter to represent regions of maxim.um time-averaged values. The anomalously warm sea surface temperatures in 1976 (Bepristis, 1977) occurred in conjunction with major circulation changes paralleling Bjerknes' (1959) hypothesis and the differences in flow regimes between a normal and dry monsoon season are in general agreement with Kanamitsu and Krishnamurti (1978). Significant correlations were found to exist between parameters within the eastern Pacific and western Pacific and also between these two regions . Particularly strong correlations involved the u², v² and IR parameters, http://archive.org/details/astudyofinterann1094528573, Captain, United States Air Force, Approved for public release; distribution is unlimited.
188. A 15-year climatology of synoptical disturbance over tropical northwestern Pacific during summer
- Author
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Chang, C.P., Chen, Jeng-Ming, Meteorology, Cheng, Chu-Chai, Chang, C.P., Chen, Jeng-Ming, Meteorology, and Cheng, Chu-Chai
- Abstract
This work investigated the sumertime northwestward propagating waves over the tropical western North Pacific and their relationship with tropical cyclone activities. The 15-season (May-October 1974-1988) Navy tropical global band data were separated into three groups according to the degree of organization in the multiple-set canonical correlation (MCC) modes that were computed from the surface v wind. Groups A (6 seasons) and B (5 seasons) showed orderly large-scale propagating patterns at the surface and 700 hPa with an average period of 8 days and a wavelength of about 2500-3000 km. The structure is robust whether the MCC analysis was performed on each of the seasons individually or on groups of years. A strong in-phase relationship between the low-level disturbance cyclonic cells and tropical cyclone centers was found. Composite analysis of all cases in these two groups whose MCC mode 1 amplitude exceeded 1.5 m/s showed organized northwestward propagating divergence/convergence patterns at 200 hPa. Group C (4 seasons) shows the least organized structure, with a large difference between MCC modes obtained from the entire group and those from each individual season. The possibility that group C contains irregular tropical cyclone tracks was discussed., http://archive.org/details/ayearclimatology1094531414, NA, NA, Republic of China (Taiwan) Navy author.
189. Upper level barotropic instability in the tropics.
- Author
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Williams, Roger T., Chang, C.P., Naval Postgraduate School (U.S.), Meteorology, Hartinger, Ronnie J., Williams, Roger T., Chang, C.P., Naval Postgraduate School (U.S.), Meteorology, and Hartinger, Ronnie J.
- Abstract
The structure of barotropically unstable disturbances in the tropics was examined with a two-level quasi-geostrophic model. The forecast equations were linearized and non-dimensionalized and the most unstable mode was found numerically by use of the initial value technique. The wind profile U(j) = a(j)U(o) sech² (y/L) was used. Simple CISK type heating was introduced to determine its effects on the growth of the waves. The jet wind profile was more unstable with easterly flow than westerly flow when no heating or friction was present. When the jet profile was present only at the upper level, the ratio of the disturbance amplitude at the lower level to the disturbance amplitude at the upper level decreased toward the equator. When the heating rate was not large enough to increase the growth rate, the amplitude ratio remained small As the heating rate becomes larger, the ratio increases to a value larger than 1., http://archive.org/details/upperlevelbarotr1094521110, Lieutenant Commander, United States Navy, Approved for public release; distribution is unlimited.
190. Hydrodynamical theory of the LO-phonon-plasmon dispersion in AlxGa1-xAs
- Author
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Fang, C.S., primary, Tse, W.S., additional, Chang, C.P., additional, Pai, K.F., additional, and Chen, Jiann-Ruey, additional
- Published
- 1988
- Full Text
- View/download PDF
191. Renal Adenocarcinoma in an Owl Monkey (Aotus trivirgatus)
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Brown, R.J., primary, Cole, W.C., additional, Chang, C.P., additional, and Hsu, S.H., additional
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- 1975
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192. A numerical study of the locally unstable barotropic easterly jet
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TUPAZ, J. B., primary, WILLIAMS, R.T., additional, and CHANG, C.P., additional
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- 1978
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193. DDT and pyrethroids: Receptor binding and mode of action in the house fly
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Chang, C.P., primary and Plapp, F.W., additional
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- 1983
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194. DDT and pyrethroids: Receptor binding in relation to knockdown resistance (kdr) in the house fly
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Chang, C.P., primary and Plapp, F.W., additional
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- 1983
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195. Enterotoxigenicity and invasive capacity of “enteropathogenic” serotypes of Escherichia coli
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Echeverria, Peter D., primary, Chang, C.P., additional, Smith, David, additional, and Anderson, Gary L., additional
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- 1976
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196. Effects of shock loading on Young's Modulus of Copper
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Chang, C.P., primary, Sinha, U.K., additional, Rai, G., additional, and Ma, C.H., additional
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- 1975
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197. The annealing behaviour of rapid solidification processed AlMo alloys
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Chang, C.P., primary and Loretto, M.H., additional
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- 1988
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198. Diffusion-induced dislocation migration in RSP AlMo
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Chang, C.P., primary and Loretto, M.H., additional
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- 1987
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199. Diffusion-induced dislocations in RSP AlMo
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Chang, C.P., primary and Loretto, M.H., additional
- Published
- 1988
- Full Text
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200. Multiple gate oxide thickness for 2 GHz system-on-a-chip technologies
- Author
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Liu, C.T., primary, Ma, Y., additional, Oh, M., additional, Diodato, P.W., additional, Stiles, K.R., additional, Mcmacken, J.R., additional, Li, F., additional, Chang, C.P., additional, Cheung, K.P., additional, Colonell, J.I., additional, Lai, W.Y.C., additional, Liu, R., additional, Lloyd, E.J., additional, Miner, J.F., additional, Pai, C.S., additional, Vaidya, H., additional, Frackoviak, J., additional, Timko, A., additional, Klemens, F., additional, Maynard, H., additional, and Clemens, J.T., additional
- Full Text
- View/download PDF
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