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1

Rattanasuk, Surachai, Rujirek Boongapim, and Tannatorn Phiwthong. "Antibacterial activity of Cathormion umbellatum." Bangladesh Journal of Pharmacology 16, no. 3 (July 13, 2021): 91–95. http://dx.doi.org/10.3329/bjp.v16i3.53420.

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The aim of this study was to determine the antibacterial activity of Cathormion umbellatum extracts against seven antibiotic-resistant bacteria. The pods, leaves and branches of C. umbellatum were extracted with ethanol and methanol. The disc diffusion assay was used to screen the antibacterial activity and broth microdilution and colorimetric assay were used to measure the minimum inhibitory concentration (MIC) and minimum bactericidal concentration (MBC) values. The result indicated that the highest inhibition zone (11 mm) was presented in ethanolic pods extract against multidrug resistance Klebsiella pneumoniae. The lowest MIC value of 0.05 mg/mL was obtained from branch extracted with ethanol against colistin resistant Pseudomonas aeruginosa. The lowest MBC values of 1.56 mg/mL were obtained when using C. umbellatum leaves extracted with methanol against all test antibiotic-resistant bacteria. This is the first report presented C. umbellatum extracts have the potential to eliminate antibiotic-resistant bacteria in patients. These findings show the antibacterial effect of C. umbellatum.
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2

Baehr, Johanna. "Influence of the 26°N RAPID–MOCHA Array and Florida Current Cable Observations on the ECCO–GODAE State Estimate." Journal of Physical Oceanography 40, no. 5 (May 1, 2010): 865–79. http://dx.doi.org/10.1175/2009jpo4118.1.

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Abstract The incorporation of local temperature and salinity observations from the Rapid Climate Change–Meridional Overturning Circulation and Heatflux Array (RAPID–MOCHA), as well as the cable estimates of volume transport in the Florida Current (FC), is tested in the Estimating the Circulation and Climate of the Ocean–Global Ocean Data Assimilation Experiment (ECCO–GODAE) estimation system for their impact on the estimate of the meridional overturning circulation (MOC) and the meridional heat transport in the Atlantic. An experimental setup covering the first deployment period of RAPID–MOCHA from March 2004 to March 2005 is used to test different strategies for incorporating these datasets. Incorporating both monthly means of the FC data and monthly means of the RAPID–MOCHA temperature and salinity measurements at the eastern and western boundaries of the basin as an observational constraint in a 1-yr experiment results in an adjustment to the reference estimate, which does not include these datasets, of approximately 1 Sv (1 Sv ≡ 106 m3 s−1) in the MOC at 26°N and the adjacent latitudes (approximately ±15°), with a larger northward branch of the MOC above 1000 m, compensated by a larger flow in the southward branch of the MOC between approximately 2000 and 3000 m. The meridional heat transport from 26°N to near 40°N is approximately 0.05 PW larger than in the reference experiment.
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3

Tandon, Neil F., Oleg A. Saenko, Mark A. Cane, and Paul J. Kushner. "Interannual Variability of the Global Meridional Overturning Circulation Dominated by Pacific Variability." Journal of Physical Oceanography 50, no. 3 (March 2020): 559–74. http://dx.doi.org/10.1175/jpo-d-19-0129.1.

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AbstractThe most prominent feature of the time-mean global meridional overturning circulation (MOC) is the Atlantic MOC (AMOC). However, interannual variability of the global MOC is shown here to be dominated by Pacific MOC (PMOC) variability over the full depth of the ocean at most latitudes. This dominance of interannual PMOC variability is robust across modern climate models and an observational state estimate. PMOC interannual variability has large-scale organization, its most prominent feature being a cross-equatorial cell spanning the tropics. Idealized experiments show that this variability is almost entirely wind driven. Interannual anomalies of zonal mean zonal wind stress produce zonally integrated Ekman transport anomalies that are larger in the Pacific Ocean than in the Atlantic Ocean, simply because the Pacific is wider than the Atlantic at most latitudes. This contrast in Ekman transport variability implies greater variability in the near-surface branch of the PMOC when compared with the near-surface branch of the AMOC. These near-surface variations in turn drive compensating flow anomalies below the Ekman layer. Because the baroclinic adjustment time is longer than a year at most latitudes, these compensating flow anomalies have baroclinic structure spanning the full depth of the ocean. Additional analysis reveals that interannual PMOC variations are the dominant contribution to interannual variations of the global meridional heat transport. There is also evidence of interaction between interannual PMOC variability and El Niño–Southern Oscillation.
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4

Hirschi, Joël J.-M., Peter D. Killworth, Jeffrey R. Blundell, and David Cromwell. "Sea Surface Height Signals as Indicators for Oceanic Meridional Mass Transports." Journal of Physical Oceanography 39, no. 3 (March 1, 2009): 581–601. http://dx.doi.org/10.1175/2008jpo3923.1.

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Abstract Numerical models are used to test whether the sea surface height (SSH) can be used as an indicator for the variability of Atlantic meridional oceanic mass transports. The results suggest that if the transports over the western boundary current region and those in the eastern part of the basin are considered separately, significant correlations (0.3–0.9) are found between zonal SSH differences and the meridional transports in the top 1100 m. Much weaker correlations are found for the basinwide transport, which corresponds to the surface branch of the meridional overturning circulation (MOC). For the eastern and western branches of the meridional transport, combining the SSH signal with the baroclinic structure obtained from Rossby wave theory enables calculation of a quantitative estimate of the transport variability in the top 1100 m. The results of the method are less convincing for the variability of the MOC. The reason for this is that even small relative errors in the variability of the eastern and western branches can be large compared with the MOC variability. These errors project onto the sum of the eastern and western transports and therefore onto the surface branch of the MOC. Nevertheless, being able to infer transport anomalies from SSH signals in the eastern and western parts of the Atlantic might prove useful in interpreting MOC observations from the U.K. Natural Environment Research Council Rapid Climate Change (RAPID) mooring array at 26°N, which show a large subannual variability that is mainly due to changes at the western boundary. Transports inferred from the SSH could help to identify the origin of this variability and whether transport anomalies propagate into the western boundary region from the basin interior or from other latitudes.
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5

Vengen, Andressa Perini, Eloisa Mattei, Carlos Augusto Rocha de Moraes Rego, Jonas Francisco Egewarth, Marinez Carpiski Sampaio, and Paulo Sérgio Rabello de Oliveira. "Atributos químicos e físicos do solo cultivado com forrageiras invernais e soja em sucessão." Agrarian 13, no. 50 (November 23, 2020): 567–477. http://dx.doi.org/10.30612/agrarian.v13i50.11832.

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Muitos produtores resistem em adotar a presença dos animais nas lavouras, pois acreditam que possa compactar o solo e causar redução na produtividade da cultura em sucessão. Diante disso, objetivou-se avaliar os atributos químicos e físicos do solo após o cultivo de forrageiras invernais sob manejos de pastejo e soja em sucessão em sistema de integração lavoura-pecuária. O experimento foi conduzido em um LATOSSOLO VERMELHO sob o delineamento de blocos ao acaso, em esquema de faixas, com três repetições. Foram testados diferentes forrageiras invernais (aveia BRS 139, aveia preta IPR 61, aveia branca IPR Esmeralda, Triticale 111 Tpolo e o consórcio de Triticale 111 TPolo e aveia IPR Esmeralda), manejos de pastejo (sem pastejo, um pastejo e dois pastejos) e profundidades do solo (0-0,05, 0,05-0,10 e 0,10-0,20 m). Foram determinados os seguintes atributos: nitrogênio total (NT), carbono orgânico total (COT), relação carbono e nitrogênio (C/N), matéria orgânica do solo (MOS), porosidade total (Pt), macroporosidade (Mac), microporosidade (Mic) e densidade aparente (Ds). As forrageiras utilizadas para pastejo no período de inverno resultaram em diferentes teores de MOS, NT e Mac. O cultivo do Triticale 111 TPolo resultou em menor Mic e Pt quando manejado sob dois pastejos nas camadas de 0,05-0,10 e 0,10-0,20 m e a maior Ds foi encontrada na camada superficial, independentemente da forrageira e manejo. As forrageiras invernais quando submetidas a pressões de pastejo não modificaram os atributos do solo entre as profundidades avaliadas.
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6

Cessi, Paola, and C. S. Jones. "Warm-Route versus Cold-Route Interbasin Exchange in the Meridional Overturning Circulation." Journal of Physical Oceanography 47, no. 8 (August 2017): 1981–97. http://dx.doi.org/10.1175/jpo-d-16-0249.1.

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AbstractThe interbasin exchange of the meridional overturning circulation (MOC) is studied in an idealized domain with two basins connected by a circumpolar channel in the southernmost region. Gnanadesikan’s conceptual model for the upper branch of the MOC is extended to include two basins of different widths connected by a reentrant channel at the southern edge and separated by two continents of different meridional extents. Its analysis illustrates the basic processes of interbasin flow exchange either through the connection at the southern tip of the long continent (cold route) or through the connection at the southern tip of the short continent (warm route). A cold-route exchange occurs when the short continent is poleward of the latitude separating the subpolar and subtropical gyre in the Southern Hemisphere (the zero Ekman pumping line); otherwise, there is warm-route exchange. The predictions of the conceptual model are compared to primitive equation computations in a domain with the same idealized geometry forced by wind stress, surface temperature relaxation, and surface salinity flux. Visualizations of the horizontal structure of the upper branch of the MOC illustrate the cold and warm routes of interbasin exchange flows. Diagnostics of the primitive equation computations show that the warm-route exchange flow is responsible for a substantial salinification of the basin where sinking occurs. This salinification is larger when the interbasin exchange is via the warm route, and it is more pronounced when the warm-route exchange flows from the wide to the narrow basin.
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7

Jones, C. S., and Paola Cessi. "Interbasin Transport of the Meridional Overturning Circulation." Journal of Physical Oceanography 46, no. 4 (April 2016): 1157–69. http://dx.doi.org/10.1175/jpo-d-15-0197.1.

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AbstractThe meridional overturning circulation (MOC) is studied in an idealized domain with two basins connected by a circumpolar channel in the southernmost region. Flow is forced at the surface by longitude-independent wind stress, freshwater flux, and fast temperature relaxation to prescribed profiles. The only longitudinal asymmetry is that one basin is twice as wide as the other. Two states, a preferred one with sinking in the narrow basin and an asymmetrically forced one with sinking in the wide basin, are compared. In both cases, sinking is compensated by upwelling everywhere else, including the passive basin. Despite the greater area of the wide basin, the residual overturning transport is the same regardless of the location of sinking. The two basins exchange flow at their southern edge by a geostrophic transport balanced by the difference in the depth of isopycnals at the eastern boundaries of each basin. Gnanadesikan’s model for the upper branch of the MOC is extended to include two basins connected by a reentrant channel and is used to illustrate the basic properties of the flow: the layer containing the surface and intermediate water is shallower in the active basin than in the passive basin, and this difference geostrophically balances an exchange flow from the passive to the active basin. The exchange flow is larger when sinking occurs in the narrow basin. A visualization of the horizontal structure of the upper branch of the MOC shows that both the gyres and the meridional flow are important in determining the flow field.
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8

Wu, Qiuyi, Yimin Yang, Mingzhong Lin, and Xiaowei Shi. "Miniaturized broadband branch-line coupler." Microwave and Optical Technology Letters 56, no. 3 (January 28, 2014): 740–43. http://dx.doi.org/10.1002/mop.28189.

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9

Bayrak, Sinehan B., J. David Kriet, and Clinton D. Humphrey. "Masseteric to buccal branch nerve transfer." Current Opinion in Otolaryngology & Head and Neck Surgery 25, no. 4 (August 2017): 280–85. http://dx.doi.org/10.1097/moo.0000000000000380.

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10

Wu, Qi, Haiming Wang, Chen Yu, Xiaowei Zhang, and Wei Hong. "Dual-band SICL branch-line coupler." Microwave and Optical Technology Letters 57, no. 5 (March 25, 2015): 1246–49. http://dx.doi.org/10.1002/mop.29062.

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11

Chongcheawchamnan, Mitchai, Sakol Julrat, Mohammad F. Shafique, Burawich Pamornak, and Ian D. Robertson. "Frequency switchable branch-line hybrid coupler." Microwave and Optical Technology Letters 55, no. 7 (April 26, 2013): 1661–63. http://dx.doi.org/10.1002/mop.27648.

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12

Jones, C. S., and Paola Cessi. "Size Matters: Another Reason Why the Atlantic Is Saltier than the Pacific." Journal of Physical Oceanography 47, no. 11 (November 2017): 2843–59. http://dx.doi.org/10.1175/jpo-d-17-0075.1.

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AbstractThe surface salinity in the North Atlantic controls the position of the sinking branch of the meridional overturning circulation (MOC); the North Atlantic has higher salinity, so deep-water formation occurs there rather than in the North Pacific. Here, it is shown that in a 3D primitive equation model of two basins of different widths connected by a reentrant channel, there is a preference for sinking in the narrow basin even under zonally uniform surface forcing. This preference is linked to the details of the velocity and salinity fields in the “sinking” basin. The southward western boundary current associated with the wind-driven subpolar gyre has higher velocity in the wide basin than in the narrow basin. It overwhelms the northward western boundary current associated with the MOC for wide-basin sinking, so freshwater is brought from the far north of the domain southward and forms a pool on the western boundary in the wide basin. The fresh pool suppresses local convection and spreads eastward, leading to low salinities in the north of the wide basin for wide-basin sinking. This pool of freshwater is much less prominent in the narrow basin for narrow-basin sinking, where the northward MOC western boundary current overcomes the southward western boundary current associated with the wind-driven subpolar gyre, bringing salty water from lower latitudes northward and enabling deep-water mass formation.
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13

Nosrati, Mehdi. "An extremely miniaturized microstrip branch-line coupler." Microwave and Optical Technology Letters 51, no. 6 (June 2009): 1403–6. http://dx.doi.org/10.1002/mop.24365.

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14

Sajadinia, Hamed, Masoud Dahmardeh, and Mohammad Khalaj-Amirhosseini. "Novel planar diplexer using branch-line coupler." Microwave and Optical Technology Letters 60, no. 11 (October 16, 2018): 2773–77. http://dx.doi.org/10.1002/mop.31484.

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15

Ye, Jiahao, Jingjing Yang, Jiang Yu, Siqiao Tan, Feng Luo, Zheming Yuan, and Yuan Chen. "A Chi-MIC Based Adaptive Multi-Branch Decision Tree." IEEE Access 9 (2021): 78962–72. http://dx.doi.org/10.1109/access.2021.3077125.

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16

Guo, Yunchuan, Yuehang Xu, and Ruimin Xu. "A Ka-band equal-branch waveguide power divider." Microwave and Optical Technology Letters 49, no. 11 (2007): 2637–39. http://dx.doi.org/10.1002/mop.22811.

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17

Yuan, Shih-Yi, Miin-Shyue Shiau, Shry-Sann Liao, Pou-Tou Sun, and Chia-Tai Ho. "An extremely compact dual-band branch-line coupler." Microwave and Optical Technology Letters 49, no. 12 (2007): 3011–14. http://dx.doi.org/10.1002/mop.22895.

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18

Noh, Y. S., M. S. Uhm, and I. B. Yom. "Compensated LTCC broadside coupler design with branch lines." Microwave and Optical Technology Letters 50, no. 12 (December 2008): 3134–36. http://dx.doi.org/10.1002/mop.23930.

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19

Kurgan, P., and M. Kitliński. "Novel doubly perforated broadband microstrip branch-line couplers." Microwave and Optical Technology Letters 51, no. 9 (June 19, 2009): 2149–52. http://dx.doi.org/10.1002/mop.24566.

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20

Yeo, S. P., and N. Deng. "Multi-section branch-line couplers for crossover application." Microwave and Optical Technology Letters 59, no. 7 (May 16, 2017): 1625–29. http://dx.doi.org/10.1002/mop.30595.

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21

Qamar, Zeeshan, Wing Shing Chan, and Ho Derek. "Wide bandwidth arbitrary phase difference branch line coupler." Microwave and Optical Technology Letters 59, no. 9 (June 27, 2017): 2241–45. http://dx.doi.org/10.1002/mop.30716.

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22

Salehi, Mohamad Reza, Leila Noori, and Ebrahim Abiri. "Novel tunable branch-line coupler for WLAN applications." Microwave and Optical Technology Letters 57, no. 5 (March 25, 2015): 1081–84. http://dx.doi.org/10.1002/mop.29025.

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23

Ali, Mohamad, S. K. A. Rahim, M. Z. M. Nor, and M. F. Jamlos. "Branch line coupler using hybrid T-model structure." Microwave and Optical Technology Letters 54, no. 1 (November 22, 2011): 237–40. http://dx.doi.org/10.1002/mop.26476.

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24

Jagadeesan, Ravi. "Cadet-Branch Matching in a Kelso-Crawford Economy." American Economic Journal: Microeconomics 11, no. 3 (August 1, 2019): 191–224. http://dx.doi.org/10.1257/mic.20170192.

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Sönmez (2013) and Sönmez and Switzer (2013) used matching theory with unilaterally substitutable priorities to propose mechanisms to match cadets to military branches. This paper shows that, alternatively, the Sönmez and Sönmez–Switzer mechanisms can be constructed as descending salary adjustment processes in Kelso-Crawford (1982) economies in which cadets are (grossly) substitutable. The lengths of service contracts serve as (inverse) salaries. The underlying substitutability explains the unilateral substitutability of the priorities utilized by Sönmez and Sönmez-Switzer. (JEL C78, D82, D86, J31, J45)
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25

Cessi, Paola. "Control of Bering Strait Transport by the Meridional Overturning Circulation." Journal of Physical Oceanography 50, no. 7 (July 1, 2020): 1853–70. http://dx.doi.org/10.1175/jpo-d-20-0026.1.

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AbstractIt is well established that the mean transport through Bering Strait is balanced by a sea level difference between the North Pacific and the Arctic Ocean, but no mechanism has been proposed to explain this sea level difference. It is argued that the sea level difference across Bering Strait, which geostrophically balances the northward throughflow, is associated with the sea level difference between the North Pacific and the North Atlantic/Arctic. In turn, the latter difference is caused by deeper middepth isopycnals in the Indo-Pacific than in the Atlantic, especially in the northern high latitudes because there is deep water formation in the Atlantic, but not in the Pacific. Because the depth of the middepth isopycnals is associated with the dynamics of the upper branch of the meridional overturning circulation (MOC), a model is formulated that quantitatively relates the sea level difference between the North Pacific and the Arctic/North Atlantic with the wind stress in the Antarctic Circumpolar region, since this forcing powers the MOC, and with the outcropping isopycnals shared between the Northern Hemisphere and the Antarctic circumpolar region, since this controls the location of deep water formation. This implies that if the sinking associated with the MOC were to occur in the North Pacific, rather than the North Atlantic, then the Bering Strait flow would reverse. These predictions, formalized in a theoretical box model, are confirmed by a series of numerical experiments in a simplified geometry of the World Ocean, forced by steady surface wind stress, temperature, and freshwater flux.
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26

Yun, Bub-Sang, Tae-Soon Yun, Jong-Chul Lee, Jong-Heon Kim, Byungje Lee, Nam-Young Kim, and Hyun-Chang Park. "CPW balanced amplifier with a new branch-line coupler." Microwave and Optical Technology Letters 39, no. 5 (October 2, 2003): 349–51. http://dx.doi.org/10.1002/mop.11213.

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27

Nguyen, Hoang V., and Christophe Caloz. "Dual-band CRLH branch-line coupler in MIM technology." Microwave and Optical Technology Letters 48, no. 11 (2006): 2331–33. http://dx.doi.org/10.1002/mop.21948.

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28

Maddah-Ali, Mohsen, Hamid Dalili Oskouei, and Keyvan Forooraghi. "A compact branch-line coupler using defected ground structures." Microwave and Optical Technology Letters 50, no. 2 (February 2008): 386–89. http://dx.doi.org/10.1002/mop.23118.

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29

Lee, Hanseung, and Sangwook Nam. "Triband branch line coupler using double-Lorentz transmission lines." Microwave and Optical Technology Letters 50, no. 5 (2008): 1174–77. http://dx.doi.org/10.1002/mop.23311.

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30

Chen, Wen-Ling, and Guang-Ming Wang. "Design of novel miniaturized fractal-shaped branch-line couplers." Microwave and Optical Technology Letters 50, no. 5 (2008): 1198–201. http://dx.doi.org/10.1002/mop.23316.

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31

Bekasiewicz, Adrian. "Miniaturized dual‐band branch‐line coupler with enhanced bandwidth." Microwave and Optical Technology Letters 61, no. 6 (February 27, 2019): 1441–44. http://dx.doi.org/10.1002/mop.31849.

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32

Salehi, Mohamadreza, and Leila Noori. "Novel 2.4 Ghz branch-line coupler using microstrip cells." Microwave and Optical Technology Letters 56, no. 9 (June 24, 2014): 2110–13. http://dx.doi.org/10.1002/mop.28552.

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33

Wu, Peng, Yong Zhang, and Qin Zhang. "A novel wideband Wilkinson divider using parallel branch lines." Microwave and Optical Technology Letters 53, no. 4 (February 22, 2011): 781–83. http://dx.doi.org/10.1002/mop.25833.

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34

Batgerel, Ariunzaya, and Soon-Young Eom. "90° branch-line Coupler with Reconfigurable Output Power Ratios." Microwave and Optical Technology Letters 55, no. 8 (May 28, 2013): 1878–81. http://dx.doi.org/10.1002/mop.27703.

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35

Soltanian, Amin, Rosy Teh, and Khai-Ming Wong. "Multi-branch structure for electrically charged four-pole axially symmetric system of solutions." International Journal of Modern Physics A 31, no. 04n05 (February 3, 2016): 1650008. http://dx.doi.org/10.1142/s0217751x16500068.

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Dyon solutions with axial symmetry in Yang–Mills–Higgs theory, including monopole–antimonopole pairs (MAP), monopole–antimonopole chains (MAC) and vortex-rings are introduced previously. The previously studied cases include at most a bifurcation for MAP systems and two for MAC dyon solutions. Here, for the case of [Formula: see text]-winding number [Formula: see text], a rich set of solutions including nine branches and four bifurcations, has been obtained for electrically charged four-pole MAC solutions. Also, the transition between two different charge configurations at a lower energy bifurcating branch is detected for the first time. This study also improves and completes some aspects of a previous study on the electrically neutral case. In the case of [Formula: see text], in addition to previously found bifurcation, another bifurcation at small values of Higgs self-coupling constant [Formula: see text], has been obtained here.
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36

Cortes-Anzures, Beatriz Olivia, Angélica María Corona-López, Víctor Hugo Toledo-Hernández, Susana Valencia-Díaz, and Alejandro Flores-Palacios. "Branch mortality influences phorophyte quality for vascular epiphytes." Botany 95, no. 7 (July 2017): 709–16. http://dx.doi.org/10.1139/cjb-2017-0023.

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Trees generate resources for other guilds (e.g., lianas), including the production of supporting branches for the establishment of epiphytes. In a tropical dry forest of central Mexico, we studied whether branch mortality is associated with phorophyte quality. For a one-year period, we monitored the survival of branches with and without vascular epiphytes in tree species with high epiphyte loads (Bursera copallifera (Sessé & Moc. Ex DC.) Bullock, Bursera glabrifolia (Kunth.) Engl.) and low (Bursera fagaroides (Kunth) Engl., Conzattia multiflora (B.L. Rob.) Standl., Ipomoea pauciflora M.Martens & Galeotti, Sapium macrocarpum Müll.Arg.). The lowest (C. multiflora) and highest (I. pauciflora) branch mortalities occurred in phorophytes with low epiphyte loads, whereas branch mortality in S. macrocarpum was 60% and in all Bursera species was <25%. In B. copallifera and B. glabrifolia, the highest branch mortality was in branches with epiphytes, suggesting a negative influence of these plants, but mortality was also associated with larger/older branches. At the end of monitoring, 95% of the epiphytes of I. pauciflora were growing on dead branches. We conclude that branch mortality is low in phorophytes with high epiphyte loads; but in phorophytes with low epiphyte loads, branches can be ephemeral or long lasting. Low epiphyte abundances in phorophytes with long-lasting branches can be caused by other traits that remain to be examined (e.g., seed capture).
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37

Palter, J. B., J. L. Sarmiento, A. Gnanadesikan, J. Simeon, and R. D. Slater. "Fueling export production: nutrient return pathways from the deep ocean and their dependence on the Meridional Overturning Circulation." Biogeosciences 7, no. 11 (November 10, 2010): 3549–68. http://dx.doi.org/10.5194/bg-7-3549-2010.

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Abstract. In the Southern Ocean, mixing and upwelling in the presence of heat and freshwater surface fluxes transform subpycnocline water to lighter densities as part of the upward branch of the Meridional Overturning Circulation (MOC). One hypothesized impact of this transformation is the restoration of nutrients to the global pycnocline, without which biological productivity at low latitudes would be significantly reduced. Here we use a novel set of modeling experiments to explore the causes and consequences of the Southern Ocean nutrient return pathway. Specifically, we quantify the contribution to global productivity of nutrients that rise from the ocean interior in the Southern Ocean, the northern high latitudes, and by mixing across the low latitude pycnocline. In addition, we evaluate how the strength of the Southern Ocean winds and the parameterizations of subgridscale processes change the dominant nutrient return pathways in the ocean. Our results suggest that nutrients upwelled from the deep ocean in the Antarctic Circumpolar Current and subducted in Subantartic Mode Water support between 33 and 75% of global export production between 30° S and 30° N. The high end of this range results from an ocean model in which the MOC is driven primarily by wind-induced Southern Ocean upwelling, a configuration favored due to its fidelity to tracer data, while the low end results from an MOC driven by high diapycnal diffusivity in the pycnocline. In all models, nutrients exported in the SAMW layer are utilized and converted rapidly (in less than 40 years) to remineralized nutrients, explaining previous modeling results that showed little influence of the drawdown of SAMW surface nutrients on atmospheric carbon concentrations.
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38

Palter, J. B., J. L. Sarmiento, A. Gnanadesikan, J. Simeon, and D. Slater. "Fueling primary productivity: nutrient return pathways from the deep ocean and their dependence on the Meridional Overturning Circulation." Biogeosciences Discussions 7, no. 3 (June 1, 2010): 4045–88. http://dx.doi.org/10.5194/bgd-7-4045-2010.

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Abstract. In the Southern Ocean, mixing and upwelling in the presence of heat and freshwater surface fluxes transform subpycnocline water to lighter densities as part of the upward branch of the Meridional Overturning Circulation (MOC). One hypothesized impact of this transformation is the restoration of nutrients to the global pycnocline, without which biological productivity at low latitudes would be catastrophically reduced. Here we use a novel set of modeling experiments to explore the causes and consequences of the Southern Ocean nutrient return pathway. Specifically, we quantify the contribution to global productivity of nutrients that rise from the ocean interior in the Southern Ocean, the northern high latitudes, and by mixing across the low latitude pycnocline. In addition, we evaluate how the strength of the Southern Ocean winds and the parameterizations of subgridscale processes change the dominant nutrient return pathways in the ocean. Our results suggest that nutrients upwelled from the deep ocean in the Antarctic Circumpolar Current and subducted in Subantartic Mode Water support between 33 and 75% of global primary productivity between 30° S and 30° N. The high end of this range results from an ocean model in which the MOC is driven primarily by wind-induced Southern Ocean upwelling, a configuration favored due to its fidelity to tracer data, while the low end results from an MOC driven by high diapycnal diffusivity in the pycnocline. In all models, the high preformed nutrients subducted in the SAMW layer are converted rapidly (in less than 40 years) to remineralized nutrients, explaining previous modeling results that showed little influence of the drawdown of SAMW surface nutrients on atmospheric carbon concentrations.
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39

Kim, TaeGyu, Byungje Lee, and Myun-Joo Park. "Dual-band branch-line coupler with two center-tapped stubs." Microwave and Optical Technology Letters 50, no. 12 (December 2008): 3136–39. http://dx.doi.org/10.1002/mop.23924.

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40

Jing, Tao, Xiao-Wei Shi, Yu-Chun Guo, Lei Chen, and Xiao-Qun Chen. "Design of a compact branch-line coupler using capacitance loading." Microwave and Optical Technology Letters 51, no. 1 (November 13, 2008): 198–200. http://dx.doi.org/10.1002/mop.23992.

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41

Chen, Wen-Ling, Guang-Ming Wang, and Chen-Xin Zhang. "Miniaturization of wideband branch-line couplers using fractal-shaped geometry." Microwave and Optical Technology Letters 51, no. 1 (November 13, 2008): 26–29. http://dx.doi.org/10.1002/mop.24002.

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42

Hosseini, F., M. Khalaj-Amir Hosseini, and M. Yazdany. "To compact ring branch-line coupler using nonuniform transmission line." Microwave and Optical Technology Letters 51, no. 11 (November 2009): 2679–82. http://dx.doi.org/10.1002/mop.24703.

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43

Gao, Liang, and Shao Yong Zheng. "A wideband 3 decibels arbitrary phase difference branch line coupler." Microwave and Optical Technology Letters 60, no. 5 (April 8, 2018): 1300–1304. http://dx.doi.org/10.1002/mop.31147.

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44

Gai, Chao, Yong-Chang Jiao, and Yu-Long Zhao. "Arbitrary power division quadrature branch-line coupler with harmonic suppression." Microwave and Optical Technology Letters 60, no. 1 (December 1, 2017): 256–60. http://dx.doi.org/10.1002/mop.30949.

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45

Velan, Sangeetha, and Malathi Kanagasabai. "Compact microstrip branch-line coupler with wideband quadrature phase balance." Microwave and Optical Technology Letters 58, no. 6 (March 28, 2016): 1369–74. http://dx.doi.org/10.1002/mop.29798.

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46

Kim, Phirun, Girdhari Chaudhary, and Yongchae Jeong. "Unequal termination branch-line balun with high-isolation wideband characteristics." Microwave and Optical Technology Letters 58, no. 8 (May 27, 2016): 1775–78. http://dx.doi.org/10.1002/mop.29914.

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47

Chen, Ja-Hao, Shih-Yi Yuan, Shi-Rong Liou, and Shry-Sann Liao. "Compact planar microstrip branch-line coupler using equal difference structure." Microwave and Optical Technology Letters 59, no. 3 (January 26, 2017): 664–68. http://dx.doi.org/10.1002/mop.30364.

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48

Ku, Chia-Hao, Lung-Kun Li, and Wei-Lung Mao. "Compact monopole antenna with branch strips for WLAN/WiMAX operation." Microwave and Optical Technology Letters 52, no. 8 (August 2010): 1858–61. http://dx.doi.org/10.1002/mop.25293.

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49

Huang, Chia-Chih, Chin-Yu Chang, and Way-Seen Wang. "Single-mode four-branch power divider with coupled wide-angle waveguides." Microwave and Optical Technology Letters 38, no. 4 (June 27, 2003): 337–41. http://dx.doi.org/10.1002/mop.11054.

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50

Huang, Chia-Chih, Chia-Chien Huang, and Way-Seen Wang. "Single-mode three-branch waveguide with a diamondlike low-index microprism." Microwave and Optical Technology Letters 45, no. 2 (2005): 145–47. http://dx.doi.org/10.1002/mop.20750.

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