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Journal articles on the topic 'JJT'

Author: Grafiati

Published: 28 May 2022

Last updated: 29 May 2022

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1

Uchiyama, Taku, Kimio Ito, Koji Mori, Hirohito Tsurumaru, and Shigeaki Harayama. "Iron-Corroding Methanogen Isolated from a Crude-Oil Storage Tank." Applied and Environmental Microbiology 76, no. 6 (2010): 1783–88. http://dx.doi.org/10.1128/aem.00668-09.

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ABSTRACT Microbiologically influenced corrosion of steel in anaerobic environments has been attributed to hydrogenotrophic microorganisms. A sludge sample collected from the bottom plate of a crude-oil storage tank was used to inoculate a medium containing iron (Fe0) granules, which was then incubated anaerobically at 37°C under an N2-CO2 atmosphere to enrich for microorganisms capable of using iron as the sole source of electrons. A methanogen, designated strain KA1, was isolated from the enrichment culture. An analysis of its 16S rRNA gene sequence revealed that strain KA1 is a Methanococcus maripaludis strain. Strain KA1 produced methane and oxidized iron much faster than did the type strain of M. maripaludis, strain JJT, which produced methane at a rate expected from the abiotic H2 production rate from iron. Scanning electron micrographs of iron coupons that had been immersed in either a KA1 culture, a JJT culture, or an aseptic medium showed that only coupons from the KA1 culture had corroded substantially, and these were covered with crystalline deposits that consisted mainly of FeCO3.

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2

Taylor, Julie. "The Academy of Breastfeeding Medicine's New 5-Year Strategic Plan (2016–2020)." Breastfeeding Medicine 11, no. 2 (2016): 94–95. http://dx.doi.org/10.1089/bfm.2016.29003.jjt.

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Taylor, Julie, and Sahira Long. "An Update from the Academy of Breastfeeding Medicine's Ethics Committee: Key Policy Revised." Breastfeeding Medicine 11, no. 3 (2016): 154–55. http://dx.doi.org/10.1089/bfm.2016.29006.jjt.

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Taylor, Julie. "Intergenerational, International Maternal–Child Health: What Is the Potential Impact of the Academy of Breastfeeding Medicine?" Breastfeeding Medicine 11, no. 4 (2016): 213–14. http://dx.doi.org/10.1089/bfm.2016.29009.jjt.

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Taylor, Julie, and Wendy Brodribb. "The Academy of Breastfeeding Medicine's Signature Product: Our Clinical Protocols." Breastfeeding Medicine 11, no. 5 (2016): 266–67. http://dx.doi.org/10.1089/bfm.2016.29011.jjt.

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6

Taylor, Julie. "World Breastfeeding Week 2016: The Academy of Breastfeeding Medicine's Important Role in Sustainable Development." Breastfeeding Medicine 11, no. 6 (2016): 328–29. http://dx.doi.org/10.1089/bfm.2016.29013.jjt.

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7

Taylor, Julie. "The Academy of Breastfeeding Medicine's Communications Committee." Breastfeeding Medicine 11, no. 7 (2016): 392–93. http://dx.doi.org/10.1089/bfm.2016.29018.jjt.

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8

Taylor, Julie, and Sarah Reece-Stremtan. "The Academy of Breastfeeding Medicine Is an International Authority: Who Are Our Partners and Allies?" Breastfeeding Medicine 12, no. 2 (2017): 125–26. http://dx.doi.org/10.1089/bfm.2016.29026.jjt.

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9

Taylor, Julie, and Eyla Boies. "Membership in the Academy of Breastfeeding Medicine: What Are the Benefits?" Breastfeeding Medicine 11, no. 9 (2016): 490–91. http://dx.doi.org/10.1089/bfm.2016.29028.jjt.

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10

Taylor, Julie. "Updates from the Academy of Breastfeeding Medicine's 2016 Annual International Meeting." Breastfeeding Medicine 11, no. 10 (2016): 564–65. http://dx.doi.org/10.1089/bfm.2016.29030.jjt.

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Taylor, Julie. "The Academy of Breastfeeding Medicine's Leadership Team for 2017." Breastfeeding Medicine 12, no. 1 (2017): 69–70. http://dx.doi.org/10.1089/bfm.2016.29033.jjt.

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Taylor, Julie, and Elien Rouw. "Strengthening the Academy of Breastfeeding Medicine's Global Identity." Breastfeeding Medicine 12, no. 3 (2017): 184–85. http://dx.doi.org/10.1089/bfm.2017.29036.jjt.

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Taylor, Julie. "The Results of an Intensive Branding Initiative? A New Web Design and Communications Tools for the Academy of Breastfeeding Medicine." Breastfeeding Medicine 12, no. 4 (2017): 247–48. http://dx.doi.org/10.1089/bfm.2017.29040.jjt.

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Taylor, Julie, and Kathy Leeper. "Educating Healthcare Providers About Breastfeeding: Something for Everyone." Breastfeeding Medicine 12, no. 5 (2017): 322–23. http://dx.doi.org/10.1089/bfm.2017.29043.jjt.

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15

Taylor, Julie. "The Many Ways to Celebrate World Breastfeeding Week 2017." Breastfeeding Medicine 12, no. 6 (2017): 386–87. http://dx.doi.org/10.1089/bfm.2017.29045.jjt.

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16

Taylor, Julie. "The History and Current Status of the Academy of Breastfeeding Medicine's Regional Network Coordinators." Breastfeeding Medicine 12, no. 7 (2017): 450–51. http://dx.doi.org/10.1089/bfm.2017.29048.jjt.

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17

Taylor, Julie. "Doctors-in-Training: The Next Generation of Leaders in Breastfeeding Medicine." Breastfeeding Medicine 12, no. 9 (2017): 577–78. http://dx.doi.org/10.1089/bfm.2017.29055.jjt.

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18

Taylor, Julie. "The Academy of Breastfeeding Medicine's Recent Past and Near Future." Breastfeeding Medicine 12, no. 10 (2017): 661–62. http://dx.doi.org/10.1089/bfm.2017.29061.jjt.

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19

Hayakawa, M., T. Horie, M. Yoshida, et al. "On the ionospheric perturbation associated with the 2007 Niigata Chuetsu-oki earthquake, as seen from subionospheric VLF/LF network observations." Natural Hazards and Earth System Sciences 8, no. 3 (2008): 573–76. http://dx.doi.org/10.5194/nhess-8-573-2008.

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Abstract. In order to investigate any precursory effect of ionospheric perturbations associated with the large 2007 Niigata Chuetsu-oki earthquake (16 July 2007) (magnitude, 6.8), we have made full use of our VLF/LF network observation in Japan by examing the four propagation paths; JJI transmitter (Kyusyu, Ebino)-MSR (Moshiri, Hokkaido), JJY transmitter (Fukushima)-MSR, JJY-KOC (Kochi) and JJI-CBA (Tateyama, Chiba). For the former two paths of JJI-MSR and JJY-MSR, we have observed significant propagation anomalies (both a decrease in nighttime average amplitude and an enhancement in nighttime amplitude fluctuation both satisfying the 2σ (σ: standard deviation) criteria) on 8–9 July, about one week before the earthquake. However, the lack of observation for the path from JJY-KOC, has enabled us to make no conclusion for this path. On the other hand, the path from JJI-CBA does not seem to be perturbed. Although this earthquake is very big and shallow, the amount of VLF anomaly for this earthquake is not so pronounced as expected, probably because the epicenter is not unfortunately located within the sensitive areas of any propagation paths. These observational facts suggest that the lower ionosphere above the epicenter is perturbed definitely prior to the earthquake, with radius of a few hundred kilometers.

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20

Abdul, Jihan A., Jimmy Posangi, Pemsi M. Wowor, and Robert A. Bara. "Uji Efek Daya Hambat Jamur Endofit Rimpang Jahe (Zingiber officinale Rosc) terhadap Bakteri Staphylococcus aureus dan Escherichia coli." Jurnal Biomedik:JBM 12, no. 2 (2020): 88. http://dx.doi.org/10.35790/jbm.12.2.2020.29163.

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Abstract: Ginger rhizome contains antimicrobial compounds of phenol group, flavonoids, terpenoids, and aetheric oil. Endophytic fungi are commonly found in ginger plant Zingiber officinale Rosc. which is widely available in Indonesia. There is a symbiosis between these endophytic fungi and its host plants in a form of genetic material transform, thus these fungi could produce the same active compounds as the host does, or at least involved in the host’s biosynthetic pathway. This study was aimed to determine the inhibitory effect of endophytic fungi isolated from ginger (Zingiber officinale Rosc) against clinical isolates Staphylococcus aureus and Escherichia coli. The endophytic fungi were isolated and their activities were screened. Initial screening of 6 isolates showed that only 3 isolates had relatively strong inhibitory effect against the bacteria. Therefore, they were cultured again, and their extracts were tested against the same types of bacteria. The mean diameters of the inhibition zones against S. aureus were, as follows: 18.7 mm (JJR extract), 11 mm (JJA 1.3 extract), and 17.3 mm (JJA 2.1 extract). Moreover, the mean diameters of the inhibition zone against E. coli were, as follows: 18 mm (JJR extract), 17.3 mm (JJA 1.3 extract), and 23.3 mm (JJA 2.1 extract). In conclusion, endophytic fungi isolated from Zingiber officinale Rosc. had inhibitory effect against S. aureus and E. coli. The inhibitory effect against E. coli was stronger than against S. aureus.Keywords: Zingiber officinale Rosc, endophytic fungi, E. coli, S. aureus Abstrak: Rimpang jahe mengandung senyawa antimikroba fenol, flavonoid, terpenoid, dan minyak atsiri. Jamur endofit sering ditemukan pada tumbuhan jahe Zingiber officinale Rosc, yang tersebar di Indonesia. Terdapat simbiosis antara jamur endofit dan tanaman inang dalam bentuk transformasi materi genetik sehingga jamur tersebut dapat menghasilkan senyawa aktif yang sama, atau setidaknya terlibat dalam jalur biosintesis inang. Penelitian ini bertujuan untuk mengetahui daya hambat jamur endofit yang terdapat pada jahe (Zingiber officinale Rosc) terhadap bakteri Staphylococcus aureus dan Escherichia coli. Jamur endofit diisolasi dan diskrining aktivitasnya. Hasil skrining awal dari 6 isolat yang diperoleh memperlihatkan hanya 3 isolat jamur endofit memiliki daya hambat yang relatif kuat terhadap bakteri uji. Ketiga isolat tersebut dikultur kembali dan ekstraknya diuji aktivitas dengan bakteri yang sama. Hasil pengukuran zona hambat 3 isolat jamur ialah sebagai berikut: pada bakteri Staphylococcus aureus didapatkan jamur JJR 18,7 mm, jamur JJA 1.3 11 mm, dan JJA 2.1 17,3 mm; pada bakteri Escherichia coli didapatkan jamur JJR 18 mm, JJA 1.3 17,3 mm, dan JJA 2.1 23,3 mm. Simpulan penelitian ini ialah jamur endofit isolat dari Zingiber officinale Rosc. memiliki aktivitas antibakteri terhadap S. aureus dan E. coli. Daya hambat jamur endofit lebih besar terhadap E. coli dibandingkan S. aureus.Kata kunci: Zingiber officinale Rosc, jamur endofitik, E. coli, S. aureus

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21

Shen, L., L. J. Mickley, and A. P. K. Tai. "Influence of synoptic patterns on surface ozone variability over the Eastern United States from 1980 to 2012." Atmospheric Chemistry and Physics Discussions 15, no. 9 (2015): 13073–108. http://dx.doi.org/10.5194/acpd-15-13073-2015.

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Abstract. We investigate the effect of synoptic-scale weather patterns on observed maximum daily 8 h average (MDA8) surface ozone over the eastern United States during 1980–2012 in summer (June–August, JJA). Zonally averaged, the SD of daily MDA8 JJA ozone shows a bimodal structure, with peaks at 30–35° N and 39–43° N, identifying those regions most influenced by daily weather variability. We apply Empirical Orthogonal Functions (EOFs) to understand the causes of this structure. The first three leading EOF patterns explain 53% of the total variance in deseasonalized surface ozone, displaying (1) a widespread decrease of ozone in the eastern United States associated with southward movement of jet wind, (2) a north–south pattern linked to the Bermuda High system when its west boundary is located along the East coast, and (3) an east–west pattern characteristic of a westward extension of Bermuda High and an enhanced Great Plains low level jet (GPLLJ). The northern peak of ozone SD can be explained by polar jet activity, while the southern peak appears related to variability in the Bermuda High and GPLLJ. In the Midwest and Northeast, we find that the correlation coefficient r between detrended mean JJA MDA8 ozone and the polar jet frequency ranges between −0.76 and −0.93 over 1980–2012 depending on the time period selected, suggesting that polar jet frequency could provide a simple metric to predict ozone variability in future climate regimes. In the Southeast, the influence of the Bermuda High on mean JJA MDA8 ozone depends on the location of its west edge. For those summers when the average position of the west edge is located west of ∼ 85.4° W, a westward shift in the Bermuda High west edge increases ozone in the Southeast by ∼ 1 ppbv deg-1 in longitude. For all summers, a northward shift in the Bermuda High west edge increases ozone over the entire eastern United States by 1–2 ppbv deg-1 in latitude. None of the synoptic patterns identified in this study show a significant trend from 1980 to 2012, confirming that the observed ozone decrease over the eastern United States during this time period is mainly caused by emission controls.

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22

Shen, L., L. J. Mickley, and A. P. K. Tai. "Influence of synoptic patterns on surface ozone variability over the eastern United States from 1980 to 2012." Atmospheric Chemistry and Physics 15, no. 19 (2015): 10925–38. http://dx.doi.org/10.5194/acp-15-10925-2015.

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Abstract. We investigate the effect of synoptic-scale weather patterns on observed maximum daily 8-hour average (MDA8) surface ozone over the eastern United States during 1980–2012 in summer (June–August, JJA). Zonally averaged, the relative standard deviation (SD) of daily MDA8 JJA ozone shows a bimodal structure, with peaks at 28–32 and 40–45° N, and we show that those regions are most influenced by the variability in daily weather. We apply empirical orthogonal functions (EOFs) to understand the causes of this structure. The first three leading EOF patterns explain 53 % of the total variance in detrended surface ozone, displaying (1) a widespread response of ozone in the eastern United States associated with north–south movement of jet wind latitude, (2) a north–south pattern linked to the Bermuda High system when its west boundary is located along the east coast, and (3) an east–west pattern characteristic of a westward extension of the Bermuda High and an enhanced Great Plains low level jet (GPLLJ). The northern peak of ozone relative SD can be explained by polar jet activity, while the southern peak appears related to variability in the Bermuda High and GPLLJ. We define a new metric polar jet frequency as the total number of days the jet traverses the Midwest and northeast each summer. In the Midwest and northeast, we find that the correlation coefficient r between detrended mean JJA MDA8 ozone and the polar jet frequency ranges between −0.76 and −0.93 over 1980–2012 depending on the time period selected, suggesting that polar jet frequency could provide a simple metric to predict ozone variability in future climate regimes. In the southeast, the influence of the Bermuda High on mean JJA MDA8 ozone depends on the location of its west edge. For those summers when the average position of the west edge is located west of ~ 85.4° W, a westward shift in the Bermuda High west edge increases ozone in the southeast by ~ 1 ppbv deg−1 in longitude. For all summers, a northward shift in the Bermuda High west edge increases ozone over the entire eastern United States by 1–2 ppbv deg−1 in latitude. None of the synoptic patterns identified in this study show a significant trend from 1980 to 2012, confirming that the observed ozone decrease over the eastern United States during this time period is mainly caused by emission controls. Our work underscores the impact of synoptic patterns on ozone variability and suggests that a combination of changing local and synoptic meteorology together with trends in background ozone will determine the influence of climate change on US ozone air quality in future decades. The observed relationships of US surface ozone and synoptic circulations in this study can also be used to validate models of atmospheric chemistry.

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23

Yang, Xiaosong, and Edmund K. M. Chang. "Eddy–Zonal Flow Feedback in the Southern Hemisphere Winter and Summer." Journal of the Atmospheric Sciences 64, no. 9 (2007): 3091–112. http://dx.doi.org/10.1175/jas4005.1.

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Abstract The eddy–zonal flow feedback in the Southern Hemisphere (SH) winter and summer is investigated in this study. The persistence time scale of the leading principal components (PCs) of the zonal-mean zonal flow shows substantial seasonal variation. In the SH summer, the persistence time scale of PC1 is significantly longer than that of PC2, while the persistence time scales of the two PCs are quite similar in the SH winter. A storm-track modeling approach is applied to demonstrate that seasonal variations of eddy–zonal flow feedback for PC1 and PC2 account for the seasonal variations of the persistence time scale. The eddy feedback time scale estimated from a storm-track model simulation and a wave-response model diagnostic shows that PC1 in June–August (JJA) and December–February (DJF), and PC2 in JJA, have significant positive eddy–mean flow feedback, while PC2 in DJF has no positive feedback. The consistency between the persistence and eddy feedback time scales for each PC suggests that the positive feedback increases the persistence of the corresponding PC, with stronger (weaker) positive feedback giving rise to a longer (shorter) persistence time scale. Eliassen–Palm flux diagnostics have been performed to demonstrate the dynamics governing the positive feedback between eddies and anomalous zonal flow. The mechanism of the positive feedback, for PC1 in JJA and DJF and PC2 in JJA, is as follows: an enhanced baroclinic wave source (heat fluxes) at a low level in the region of positive wind anomalies propagates upward and then equatorward from the wave source, thus giving momentum fluxes that reinforce the wind anomalies. The difference of PC2 between DJF and JJA is because of the zonal asymmetry of the climatological flow in JJA. For PC2 in DJF, wind anomalies reinforce the climatological jet, thus increasing the barotropic shear of the jet flow. The “barotropic governor” plays an important role in suppressing eddy generations for PC2 in DJF and thus inhibiting the positive eddy–zonal flow feedback.

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24

Song, Jie, Chongyin Li, Jing Pan, and Wen Zhou. "Climatology of Anticyclonic and Cyclonic Rossby Wave Breaking on the Dynamical Tropopause in the Southern Hemisphere." Journal of Climate 24, no. 4 (2011): 1239–51. http://dx.doi.org/10.1175/2010jcli3157.1.

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Abstract The characteristics of the climatological distribution of the anticyclonic (LC1) and cyclonic (LC2) Rossby wave breaking (RWB) in the Southern Hemisphere (SH) are investigated by calculating the occurrence frequency of the LC1- and LC2-like stratospheric potential vorticity (PV) streamers in the SH during the austral summer [December–February (DJF)] and wintertime [June–August (JJA)] on several isentropic surfaces by using the 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) daily dataset. The results show that 1) on the equatorward flank of the climatological midlatitude jet (MLJ), the LC1-like PV streamers are frequently found over the central oceanic regions, whereas the LC2-like PV streamers are almost absent. On the poleward flank of the climatological MLJ, both types of PV streamers are frequently observed and the LC2-like PV streamers predominate; 2) the regions where the occurrences of the PV streamers are frequent overlap the weak zonal wind regions; and 3) in austral winter, a “double-jet” setting is evident in two regions of the SH [the double-jet upstream (DU) and the spilt jet region]. In the double-jet setting regions, the LC1-like PV streamers are frequently found both in the DU and the split-jet regions, while the occurrence of the LC2-like PV streamers is frequent in the split-jet region but is rather infrequent in the DU region.

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25

Albern, Nicole, Aiko Voigt, David W. J. Thompson, and Joaquim G. Pinto. "The Role of Tropical, Midlatitude, and Polar Cloud-Radiative Changes for the Midlatitude Circulation Response to Global Warming." Journal of Climate 33, no. 18 (2020): 7927–43. http://dx.doi.org/10.1175/jcli-d-20-0073.1.

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AbstractPrevious studies showed that global cloud-radiative changes contribute half or more to the midlatitude atmospheric circulation response to global warming. Here, we investigate the relative importance of tropical, midlatitude, and polar cloud-radiative changes for the annual-mean, wintertime, and summertime circulation response across regions in AMIP-like simulations. To this end, we study global warming simulations from the ICON model run with the cloud-locking method and prescribed sea surface temperatures, which isolate the impact of changes in atmospheric cloud-radiative heating. Tropical cloud changes dominate the global cloud impact on the 850 hPa zonal wind, jet strength, and storm track responses across most seasons and regions. For the jet shift, a more diverse picture is found. In the annual mean and DJF, tropical and midlatitude cloud changes contribute substantially to the poleward jet shift in all regions. The poleward jet shift is further supported by polar cloud changes across the Northern Hemisphere but not in the Southern Hemisphere. In JJA, the impact of regional cloud changes on the jet position is small, consistent with an overall small jet shift during this season. The jet shift can be largely understood via the anomalous atmospheric cloud-radiative heating in the tropical and midlatitude upper troposphere. The circulation changes are broadly consistent with the influence of cloud-radiative changes on upper-tropospheric baroclinicity and thus the mean potential energy available for conversion into eddy kinetic energy. Our results help to explain the jet response to global warming and highlight the importance of tropical and midlatitude cloud-radiative changes for this response.

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26

Wilson, Aaron B., David H. Bromwich, and Keith M. Hines. "Simulating the Mutual Forcing of Anomalous High Southern Latitude Atmospheric Circulation by El Niño Flavors and the Southern Annular Mode*." Journal of Climate 29, no. 6 (2016): 2291–309. http://dx.doi.org/10.1175/jcli-d-15-0361.1.

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Abstract Numerical simulations using the National Center for Atmospheric Research Community Atmosphere Model (CAM) are conducted based on tropical forcing of El Niño flavors. Though these events occur on a continuum, two general types are simulated based on sea surface temperature anomalies located in the central (CP) or eastern (EP) tropical Pacific. The goal is to assess whether CAM adequately represents the transient eddy dynamics associated with each of these El Niño flavors under different southern annular mode (SAM) regimes. CAM captures well the wide spatial and temporal variability associated with the SAM but only accurately simulates the impacts on atmospheric circulation in the high southern latitudes when the observed SAM phase is matched by the model. Composites of in-phase (El Niño–SAM−) and out-of-phase (El Niño–SAM+) events confirm a seasonal preference for in-phase (out of phase) events during December–February (DJF) [June–August (JJA)]. Modeled in-phase events for both EP (during DJF) and CP (during JJA) conditions support observations of anomalous equatorward momentum flux on the equatorward side of the eddy-driven jet, shifting this jet equatorward and consistent with the low phase of the SAM. Out-of-phase composites show that the El Niño–associated teleconnection to the high southern latitudes is strongly modulated by the SAM, as a strong eddy-driven jet is well maintained by high-latitude transient eddy convergence despite the tropical forcing. A regional perspective confirms that this interaction takes place primarily over the Pacific Ocean, with high-latitude circulation variability being a product of both tropical and high-latitude forcing.

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27

HARADA, Ikuko. "Journal coverage comparison between JST and foreign major databases." Journal of Information Processing and Management 47, no. 2 (2004): 96–101. http://dx.doi.org/10.1241/johokanri.47.96.

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MIYAGAWA, Yoshiyuki. "JST Training Program for Specialists of Technology Transfer." Journal of Information Processing and Management 48, no. 1 (2005): 32–39. http://dx.doi.org/10.1241/johokanri.48.32.

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Builes-Jaramillo, Alejandro, Johanna Yepes, and Hernán D. Salas. "The Orinoco Low-Level Jet and Its Association with the Hydroclimatology of Northern South America." Journal of Hydrometeorology 23, no. 2 (2022): 209–23. http://dx.doi.org/10.1175/jhm-d-21-0073.1.

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Abstract We investigated the relationship between the frequency of occurrence of the Orinoco low-level jet (OLLJ) and hydroclimatic variables over northern South America. We use data from the ERA5 atmospheric reanalysis to characterize the spatial and temporal variability of the OLLJ in light of the low-level jet (LLJ) classification criteria available in the literature. An index for the frequency of occurrence of an LLJ was used, based on the hourly maxima of wind speed. The linkages among the OLLJ, water vapor flux, and precipitation were analyzed using a composite analysis. Our results show that during December–February (DJF), the OLLJ exhibits its maximum wind speed, with values around 8–10 m s−1. During DJF, the analysis shows how the OLLJ transports atmospheric moisture from the tropical North Atlantic Ocean. During this season, the predominant pathway of the OLLJ is associated with an area of moisture flux divergence located over northeastern South America. During June–August (JJA), an area of moisture flux convergence associated with the northernmost location of the ITCZ inhibits the entrance of moisture from northerlies. We also show that the occurrence of the OLLJ is associated with the so-called cross-equatorial flow. During DJF, the period of strongest activity of the OLLJ is associated with the northerly cross-equatorial flow and dry season, whereas during JJA the southerly cross-equatorial flow from the Amazon River basin predominates and contributes to the rainy season over the Orinoco region.

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30

ARAI, Noriyuki. "No.15: Patent supporting system in JST." Journal of Information Processing and Management 47, no. 5 (2004): 348–57. http://dx.doi.org/10.1241/johokanri.47.348.

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31

FASSOULIOTIS, DIMITRIS. "CHARGED TGC FROM 1999 DELPHI DATA." International Journal of Modern Physics A 16, supp01a (2001): 299–301. http://dx.doi.org/10.1142/s0217751x01006747.

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Measurements of the trilinear gauge boson couplings WWγ and WWZ are presented from data taken by DELPHI in 1999 at an energy ranging from 192 to 202 GeV. Values are extracted with respect to [Formula: see text] and Δ κγ, the differences of the WWZ charge coupling and of the WWγ dipole coupling from their Standard Model values, and λγ, the WWγ quadrupole coupling. The study uses data from the final states jjℓν, jjjj, ℓX, jjX and γX, where j represents a quark jet, l an identified lepton and X missing four-momentum. The observations are consistent with the Standard Model predictions.

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WATANABE, Daisuke, Hiroshi MAEKAWA, and Yuichi MATSUO. "SUPERSONIC PLANE JET AT HIGHT CONVECTIVE MACH NUMBER(Plane Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 189–94. http://dx.doi.org/10.1299/jsmeicjwsf.2005.189.

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33

Tabata, Takahide, Satoshi Someya, and Masahiro Nakashima. "JET FLOW ISSUING UPWARD WITH SUBSTANCE DIFFUSION(Jet and Plume)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 399–404. http://dx.doi.org/10.1299/jsmeicjwsf.2005.399.

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Sato, Hiroshi, Hirofumi Hattori, and Yasutaka Nagano. "TURBULENCE MODEL FOR PREDICTING HEAT TRANSFER IN IMPINGING JET(Impinging Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 117–22. http://dx.doi.org/10.1299/jsmeicjwsf.2005.117.

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Yasunobu, Tsuyoshi, Yumiko Otobe, Hideo Kashimura, and Toshiaki Setoguchi. "CHARACTERISTICS OF OSCILLATION FREQUENCY CAUSED BY SUPERSONIC IMPINGING JET(Impinging Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 123–28. http://dx.doi.org/10.1299/jsmeicjwsf.2005.123.

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36

Makita, Hideharu, and Nobumasa Sekishita. "MECHANISM OF VORTEX PAIRING IN A PARABOLIC PLANE JET(Plane Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 177–82. http://dx.doi.org/10.1299/jsmeicjwsf.2005.177.

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Narabayashi, Tadashi, Yukitaka Yamazaki, Hidetoshi Kobayashi, and Toshihiko Shakouchi. "Flow Analysis for Single and Multi-Nozzle Jet Pump(Multiple Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 267–72. http://dx.doi.org/10.1299/jsmeicjwsf.2005.267.

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38

Ichimiya, Koichi, and Koji Tsukamoto. "HEAT TRANSFER FROM AN INFLOW-TYPE SWIRLING TURBULENT IMPINGING JET(Impinging Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 111–16. http://dx.doi.org/10.1299/jsmeicjwsf.2005.111.

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SHIMIZU, Fumio, Kazuhiro TANAKA, and Kimishiro TOKUDA. "EXPERIMENTAL STUDY OF SIPHON PHENOMENON INDUCED BY A WATER JET(Water Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 333–36. http://dx.doi.org/10.1299/jsmeicjwsf.2005.333.

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40

Deo, R. C., J. Mi, and G. J. Nathan. "DEPENDENCE OF A PLANE TURBULENT JET ON ITS NOZZLE CONTRACTION PROFILE(Plane Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 183–88. http://dx.doi.org/10.1299/jsmeicjwsf.2005.183.

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41

Alekseenko, Sergey, Artur Bilsky, Vladimir Dulin, Boris Ilyushin, and Dmitriy Markovich. "TURBULENT ENERGY BALANCE IN FREE AND CONFINED JET FLOWS(Free and Confined Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 281–86. http://dx.doi.org/10.1299/jsmeicjwsf.2005.281.

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42

SHIMIZU, Seiji, Takatoshi NISHIYAMA, and Hiroaki KATO. "EFFECTIVENESS OF SHEATHED ABRASIVE WATER SUSPENSION JET NOZZLE FOR SUBMERGED APPLICATION(Water Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 349–54. http://dx.doi.org/10.1299/jsmeicjwsf.2005.349.

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43

Peng, Guoyi. "NUMERICAL STUDY OF CAVITATING VORTEX FLOW IN STARTING SUBMERGED WATER JET(Water Jet)." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2005 (2005): 355–60. http://dx.doi.org/10.1299/jsmeicjwsf.2005.355.

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44

Silva, Gyrlene A. M., Lívia M. M. Dutra, Rosmeri P. da Rocha, Tércio Ambrizzi, and Érico Leiva. "Preliminary Analysis on the Global Features of the NCEP CFSv2 Seasonal Hindcasts." Advances in Meteorology 2014 (2014): 1–21. http://dx.doi.org/10.1155/2014/695067.

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The representation of the CFSv2 ocean-atmosphere ensemble hindcasts is investigated during Dec-Jan-Feb (DJF) and Jun-Jul-Aug (JJA) from 1983 to 2010. The skill anomaly correlations showed that in some continents the forecasts do not have dependency with changes in the initial conditions. Also, in both seasons the model has a higher skill at the 0-month lead time with the largest spatial biases occurring over the North America, South America, and Oceania. Over the continents the largest biases in the nonlinearity of El Niño minus La Niña events are found over the eastern South Africa, part of Oceania, and central-southeastern parts of South America. During DJF the main biases are related to double-ITCZ, strengthening of SPCZ, and deepening of the Aleutian and Icelandic low pressures. The simulation of a warmer SST on the eastern of most austral oceans, the strengthening (weakening) of the Subtropical (Polar) Jet over the Southern Hemisphere, and the weakening of the zonal circulation near the Antarctic continent are also found in both seasons. Over the central-eastern Equatorial Pacific a cooler bias in SST is found during JJA. These biases are interpreted by analyses of the simulated global mean-state and their impact on the main patterns of variability.

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Aguirre, Catalina, Valentina Flores-Aqueveque, Pablo Vilches, Alicia Vásquez, José A. Rutllant, and René Garreaud. "Recent Changes in the Low-Level Jet along the Subtropical West Coast of South America." Atmosphere 12, no. 4 (2021): 465. http://dx.doi.org/10.3390/atmos12040465.

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Surface winds along the subtropical west coast of South America are characterized by the quasi-weekly occurrences of low-level jet events. These short lived but intense wind events impact the coastal ocean environment. Hence, identifying long-term trends in the coastal low-level jet (CLLJ) is essential for understanding changes in marine ecosystems. Here we use ERA5 reanalysis (1979–2019) and an objective algorithm to track anticyclones to investigate recent changes in CLLJ events off central Chile (25–43 °S). Results present evidence that the number of days with intense wind (≥10 ms−1), and the number and duration of CLLJ events have significantly changed off central Chile in recent decades. There is an increase in the number of CLLJ events in the whole study area during winter (June-July-August; JJA), while during summer (December–January–February; DJF) a decrease is observed at lower latitudes (29–34 °S), and an increase is found at the southern boundary of the Humboldt system. We suggest that changes in the central pressures and frequency of extratropical, migratory anticyclones that reach the coast of South America, which force CLLJs, have played an important role in the recent CLLJ changes observed in this region.

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Tanaka, I., N. Watanabe, Y. Ito, T. Nakajima, K. Saito, and A. Nakamura. "New Tomei Expressway (Gotemba JCT～Inasa JCT)." Concrete Journal 49, no. 1 (2011): 1_43–1_60. http://dx.doi.org/10.3151/coj.49.1_43.

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Yutaka, Oda, and Takeishi Kenichiro. "1179 ENHANCEMENT OF JET IMPINGEMENT HEAT TRANSFER WITH RIB TURBULATORS IN WALL JET REGION." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2013.4 (2013): _1179–1_—_1179–6_. http://dx.doi.org/10.1299/jsmeicjwsf.2013.4._1179-1_.

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48

Djauhari, Achmad. "Analisa Finansial Usahatani Pepaya Bangkok dan Tanaman Alternatif di Lahan Kering: Studi Kasus Empat Desa di Kabupaten Malang." Forum penelitian Agro Ekonomi 1, no. 2 (2016): 63. http://dx.doi.org/10.21082/fae.v1n2.1983.63-70.

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<strong>Indonesian</strong><br />Dengan adanya impor beberapa jenis buah-buahan, merupakan salah satu indikator bahwa kita belum dapat menghasilkan dengan baik, terutama masalah kualitas yang sesuai dengan selera konsumen. Oleh karenanya dalam usaha pengembangan tanaman buah-buahan dipandang perlu dilakukan penelitian sebagai suplemen terhadap penelitian teknis agronomis. Tulisan ini membahas kelayakan finansial usahatani tanaman pepaya bangkok apabila digantikan dengan beberapa tanaman alternatif. Sebagai tanaman alternatif adalah pola pergiliran tanaman setahun yang terdiri dari beberapa pola: (a) Pola, Jagung - jagung - kacang tanah (JJK) (b) Pola, Jagung - jagung - jagung (JJJ) dan (c) Pola, Jagung - kacang tanah - kacang tanah (JKK). Dengan menggunakan kriteria investasi BCR dan IRR, telah memberikan petunjuk yang mantap bahwa pengusahaan tanaman pepaya mampu memberikan tambahan penerimaan sampai 50 persen di atas tambahan biaya yang harus dikeluarkan.

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RADWAN, AHMED E. "ALFVEN SURFACE WAVES ALONG ANNULAR GAS JET SURROUNDING TAR COLUMN UNDER OBLIQUE VARYING MAGNETIC FIELD." Tamkang Journal of Mathematics 28, no. 2 (1997): 127–33. http://dx.doi.org/10.5556/j.tkjm.28.1997.4326.

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The MFD oscillating Alfven surface waves along a perfectly conducting annular gas jct surrounding a tar column under oblique varying magnetic field has been discussed. Numerous reported works could be recovered as limiting cases. The axial magnetic fields interior and exterior the model are stabilizing while the tenuous azimuthal field is so or not according to restrictions. The thicker the tar column the larger its stabilizing influence; and the oscillation states arc slowed down so easier observations are allowed than in the classical case of full fluid jet in vacuum with constant magnetic fields (Uberio and Somasundaram 1980). The Alfven wave velocity is decreasing with increasing azimuthal-longitudinal magnetic fields intensities ratio. The phase (dispersive) velocity of the wave propagation relative to Alfven wave velocity is monotonic increasing with decreasing the perturbed wavelength.

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Solsjo, R., M. Jangi, C. Chartier, O. Andersson, and X. S. Bai. "HC1-3 Jet-Jet Interaction in Diesel Engine Combustion(HC: HCCI Combustion,General Session Papers)." Proceedings of the International symposium on diagnostics and modeling of combustion in internal combustion engines 2012.8 (2012): 398–403. http://dx.doi.org/10.1299/jmsesdm.2012.8.398.

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