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1

Correia dos Santos, Eliete, and Wiliana De Araújo Borges. "SESA ON-LINE." Archeion Online 9, no. 1 (June 15, 2021): 110–14. http://dx.doi.org/10.22478/ufpb.2318-6186.2021v9n1.59399.

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A palestra “Representação documental no contexto da arquivologia” apresentada por Barros (2020) pelo projeto SESA-ON-LINE abordou os processos de representação que fazem parte do cotidiano dos arquivos, bibliotecas e museus. No primeiro momento, buscou-se através do universo dos arquivos apropriar-se das discussões relacionadas à representação e à organização da informação e do conhecimento; em seguida, discutiu-se a respeito do percurso do conceito de representação sob dois eixos: no contexto da organização depois no contexto da arquivologia, com a intenção de sistematizar as várias facetas do conceito de representação e aproximar dos processos arquivísticos, visando um aprimoramento dos processos classificatórios e descritivos em Arquivologia.
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2

Martín-Gómez, Verónica, Emilio Hernández-Garcia, Marcelo Barreiro, and Cristóbal López. "Interdecadal Variability of Southeastern South America Rainfall and Moisture Sources during the Austral Summertime." Journal of Climate 29, no. 18 (September 1, 2016): 6751–63. http://dx.doi.org/10.1175/jcli-d-15-0803.1.

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Abstract Sea surface temperature (SST) anomalies over the tropical oceans are able to generate extratropical atmospheric circulation anomalies that can induce rainfall variability and changes in the sources of moisture. The work reported here evaluates the interdecadal changes in the moisture sources for southeastern South America (SESA) during austral summer, and it is divided into two complementary parts. In the first part the authors construct a climate network to detect synchronization periods among the tropical oceans and the precipitation over SESA. Afterward, taking into account these results, the authors select two periods with different degrees of synchronization to compare the spatial distribution of the SESA moisture sources. Results show that during the last century there were three synchronization periods among the tropical oceans and the precipitation over SESA (during the 1930s, 1970s, and 1990s) and suggest that the main moisture sources of SESA are the recycling over the region, the central-eastern shore of Brazil together with the surrounding Atlantic Ocean, and the southwestern South Atlantic surrounding the SESA domain. Comparison of SESA moisture sources for the 1980s (a period of nonsignificant synchronization) and the 1990s (a synchronized period) shows that the principal differences are in the intensity of the recycling and in the strength of the central-eastern shore of Brazil. Moreover, the authors find that a region centered at (20°S, 300°E) is a moisture source for SESA only during the 1990s. These differences can be associated with the development of a low-level anticyclonic (cyclonic) anomaly circulation over central-eastern Brazil that favors the transport of moisture from central Brazil (central-eastern shore of Brazil) toward SESA in the 1990s (1980s).
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3

Kumano, Takuto, Etsuko Fujiki, Yoshiteru Hashimoto, and Michihiko Kobayashi. "Discovery of a sesamin-metabolizing microorganism and a new enzyme." Proceedings of the National Academy of Sciences 113, no. 32 (July 21, 2016): 9087–92. http://dx.doi.org/10.1073/pnas.1605050113.

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Sesamin is one of the major lignans found in sesame oil. Although some microbial metabolites of sesamin have been identified, sesamin-metabolic pathways remain uncharacterized at both the enzyme and gene levels. Here, we isolated microorganisms growing on sesamin as a sole-carbon source. One microorganism showing significant sesamin-degrading activity was identified asSinomonassp. no. 22. A sesamin-metabolizing enzyme named SesA was purified from this strain and characterized. SesA catalyzed methylene group transfer from sesamin or sesamin monocatechol to tetrahydrofolate (THF) with ring cleavage, yielding sesamin mono- or di-catechol and 5,10-methylenetetrahydrofolate. The kinetic parameters of SesA were determined to be as follows:Kmfor sesamin = 0.032 ± 0.005 mM,Vmax= 9.3 ± 0.4 (μmol⋅min−1⋅mg−1), andkcat= 7.9 ± 0.3 s−1. Next, we investigated the substrate specificity. SesA also showed enzymatic activity toward (+)-episesamin, (−)-asarinin, sesaminol, (+)-sesamolin, and piperine. Growth studies with strain no. 22, and Western blot analysis revealed that SesA formation is inducible by sesamin. The deduced amino acid sequence ofsesAexhibited weak overall sequence similarity to that of the protein family of glycine cleavage T-proteins (GcvTs), which catalyze glycine degradation in most bacteria, archaea, and all eukaryotes. Only SesA catalyzes C1 transfer to THF with ring cleavage reaction among GcvT family proteins. Moreover, SesA homolog genes are found in both Gram-positive and Gram-negative bacteria. Our findings provide new insights into microbial sesamin metabolism and the function of GcvT family proteins.
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4

Seager, Richard, Naomi Naik, Walter Baethgen, Andrew Robertson, Yochanan Kushnir, Jennifer Nakamura, and Stephanie Jurburg. "Tropical Oceanic Causes of Interannual to Multidecadal Precipitation Variability in Southeast South America over the Past Century*." Journal of Climate 23, no. 20 (October 15, 2010): 5517–39. http://dx.doi.org/10.1175/2010jcli3578.1.

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Abstract Observations, atmosphere models forced by historical SSTs, and idealized simulations are used to determine the causes and mechanisms of interannual to multidecadal precipitation anomalies over southeast South America (SESA) since 1901. About 40% of SESA precipitation variability over this period can be accounted for by global SST forcing. Both the tropical Pacific and Atlantic Oceans share the driving of SESA precipitation, with the latter contributing the most on multidecadal time scales and explaining a wetting trend from the early midcentury until the end of the last century. Cold tropical Atlantic SST anomalies are shown to drive wet conditions in SESA. The dynamics that link SESA precipitation to tropical Atlantic SST anomalies are explored. Cold tropical Atlantic SST anomalies force equatorward-flowing upper-tropospheric flow to the southeast of the tropical heating anomaly, and the vorticity advection by this flow is balanced by vortex stretching and ascent, which drives the increased precipitation. The 1930s Pampas Dust Bowl drought occurred, via this mechanism, in response to warm tropical Atlantic SST anomalies. The atmospheric response to cold tropical Pacific SSTs also contributed. The tropical Atlantic SST anomalies linked to SESA precipitation are the tropical components of the Atlantic multidecadal oscillation. There is little evidence that the large trends over past decades are related to anthropogenic radiative forcing, although models project that this will cause a modest wetting of the climate of SESA. As such, and if the Atlantic multidecadal oscillation has shifted toward a warm phase, it should not be assumed that the long-term wetting trend in SESA will continue. Any reversal to a drier climate more typical of earlier decades would have clear consequences for regional agriculture and water resources.
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5

Wu, Yutian, and Lorenzo M. Polvani. "Recent Trends in Extreme Precipitation and Temperature over Southeastern South America: The Dominant Role of Stratospheric Ozone Depletion in the CESM Large Ensemble." Journal of Climate 30, no. 16 (July 19, 2017): 6433–41. http://dx.doi.org/10.1175/jcli-d-17-0124.1.

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Abstract Observations show an increase in maximum precipitation extremes and a decrease in maximum temperature extremes over southeastern South America (SESA) in the second half of the twentieth century. The Community Earth System Model (CESM) Large Ensemble (LE) experiments are able to successfully reproduce the observed trends of extreme precipitation and temperature over SESA. Careful analysis of a smaller ensemble of CESM-LE single forcing experiments reveals that the trends of extreme precipitation and temperature over SESA are mostly caused by stratospheric ozone depletion. The underlying dynamical mechanism is investigated and it is found that, as a consequence of stratospheric ozone depletion and the resulting southward shift of tropospheric jet streams, anomalous easterly flow and more intense cyclones have occurred over SESA, which are favorable for heavier rainfall extremes and milder heat extremes.
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6

Kaplan, Peter W., Andrew Billnitzer, and José Luis Fernández-Torre. "Subacute Encephalopathy With Seizures in Alcoholics (SESA) Presenting as Focal Nonconvulsive Status Epilepticus." Clinical EEG and Neuroscience 49, no. 6 (December 20, 2017): 414–16. http://dx.doi.org/10.1177/1550059417747435.

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Purpose. To acquaint readers with the underrecognized subacute encephalopathy with seizures in chronic alcoholics (SESA) that has more recently been associated with different types of status epilepticus. Methods. Case reports and review of the literature on SESA and nonconvulsive status epilepticus (NCSE). Results. Two cases: one with alternating bifrontoparietal NCSE, and one with focal, confusional NCSE, with imaging and EEG correlates. Conclusion. Underrecognized SESA may present as NCSE with focal clinical, EEG and reversible diffusion-weighted MRI abnormalities, warranting expedited diagnosis and antiseizure treatment to minimize morbidity.
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7

Setyowati, Riris, and Pribowo Angling Kusumo. "ANALISIS LEVEL OF SERVICE (L.O.S): STUDI KASUS DI JALAN DRS. ESAU SESA, KABUPATEN MANOKWARI, PROVINSI PAPUA BARAT." INTAN Jurnal Penelitian Tambang 4, no. 1 (April 1, 2022): 24–30. http://dx.doi.org/10.56139/intan.v4i1.78.

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Jalan Drs. Esau Sesa is a non-shared two-way connecting road owned by the Manokwari Regency Government, Papua Barat Province. This road is the main road that connects between districts with a road width of + 6 meters. The rapid development of land use along with Drs. Esau Sesa has the potential to reduce road service levels. Field observations showed that commercial activities are high in this area. Thus the traffic activities, as well as parked vehicles are also high, exceeding the facilities capacities. This condition is one of the causes of traffic jams on the road. Based on the data analysis results, Jalan Drs. Esau Sesa has a Road Capacity (C) of 2,061 vehicles/hour with a Free Flow Velocity (FV) of 45,315 Km/hour and a Degree of Saturation (DS) of 0.808. These results are equivalent to the Level of Service (L.O.S) at level D which means traffic flow on Jalan Dr. Esau Sesa began to become unstable, with low traffic jams with creeping currents and vehicle volumes approaching maximum capacity.
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8

Vitvar, Tomas, Michal Zaremba, Matthew Moran, Maciej Zaremba, and Dieter Fensel. "SESA: Emerging Technology for Service-Centric Environments." IEEE Software 24, no. 6 (November 2007): 56–67. http://dx.doi.org/10.1109/ms.2007.178.

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9

Gomes, Liliana Isabel Esteves, and Maria Beatriz Marques. "IX Seminário Internacional de Saberes Arquivísticos (SESA)." Archeion Online 7, no. 1 (December 23, 2019): 1–3. http://dx.doi.org/10.22478/ufpb.2318-6186.2019v7n1.49812.

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10

Taylor, C. E. "Benjamin J. Lazan: SESA President 1959-1960." Experimental Techniques 23, no. 6 (November 1999): 25–29. http://dx.doi.org/10.1111/j.1747-1567.1999.tb01314.x.

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11

Putu Budiadnya and Dewa Nyoman Putra Adnyana. "NILAI NILAI ETIKA DALAM YADNYA SESA BAGI KEHIDUPAN KESEHARIAN UMAT HINDU DI SURAKARTA." Widya Aksara : Jurnal Agama Hindu 26, no. 2 (September 27, 2021): 159–78. http://dx.doi.org/10.54714/widyaaksara.v26i2.160.

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Alam semesta dengan segala bentuk ciptaan sebenarnya telah diciptakan melalui proses Yadnya. Karena itu semua yang ada di alam semesta ini juga ditopang oleh Yadnya. Artinya tanpa Yadnya tidak akan pernah ada kehidupan, demikian pula tanpa Yadnya alam semesta ini pasti mengalami kehancuran. Pengertian Yadnya itu sendiri adalah pengorbanan yang tulus dan suci, oleh sebab itu, salah satu kegiatan umat Hindu di dalam menghayati agamanya adalah melalui pelaksanaan Yadnya Sesa. Berdasarkan sastra dan tradisi dalam ajaran agama Hindu, ditemukan petunjuk yang kuat mengenai sarana upacara Yadnya, yang merupakan ciri khas yang kuat di dalam pelaksanaan upacara Yadnya Sesa, antara lain di tempat memasak, di tempat penyimpanan air, di atas genteng, di halaman dan di tugu/tempat suci Upacara Yadnya Sesa adalah salah satu bentuk Bhuta Yadnya dan manifestasi dari Panca Yadnya yang dilakukan setiap hari (nitya karma) yaitu sehabis memasak di dapur umat Hindu memberikan atau menghaturkan makanan persembahan (banten) sebagai sebuah perwujudan kasih sayang terhadap semua atau sesama makhluk di alam semesta (sarwa prani) dan manifestasi sadhana (bhakti yang terus menerus) kepada Sang Hyang Widhi Wasa menyikapi rasa syukur atas nikmat dan kemurahan rezeki yang diberikan-Nya setiap hari. Yadnya Sesa yang banyak mengandung makna bagi kehidupan umat Hindu diyakini dapat membimbing umat kepada tumbuhnya jiwa sosial, harmonis dan toleran dalam hidup berdampingan dengan sesama makhluk serta menanamkan rasa kasih sayang dan rasa terima kasih atas anugerah Tuhan, Yadnya Sesa hanya mampu dijelaskan dengan bahasa hati dan hanya dapat dipahami oleh orang yang melaksanakannya.
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12

Zamboni, Laura, Carlos R. Mechoso, and Fred Kucharski. "Relationships between Upper-Level Circulation over South America and Rainfall over Southeastern South America: A Physical Base for Seasonal Predictions." Journal of Climate 23, no. 12 (June 15, 2010): 3300–3315. http://dx.doi.org/10.1175/2009jcli3129.1.

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Abstract The existence of a significant simultaneous correlation between bimonthly mean precipitation anomalies over southeastern South America (SESA) and either the first or the second (depending on season) leading mode of interannual variability of upper-level wind over South America (SA) is demonstrated during all seasons except winter. The pattern associated with these modes of variability is similar during all seasons and consists of a continental-scale vortex centered over the eastern coast of subtropical SA. The vortex has a quasi-barotropic structure during all seasons, and its variability modifies moisture transport from the South American low-level jet and the western tropical Atlantic to SESA thus creating precipitation anomalies in this region. During spring (October–November) and summer (January–February) the circulation creates a second center of precipitation anomalies over the South Atlantic convergence zone that are of opposite sign to those over SESA, while during fall (April–May) precipitation anomalies are primarily confined to SESA. On the basis of the correlation between upper-level winds and precipitation, an empirical method to produce long-range forecasts of bimonthly mean precipitation over SESA is developed. Method tests in hindcast mode for the period 1959–2001 show a potential for reliable predictions during the southern spring, summer, and fall. The method is further tested in an experimental mode by using Development of a European Multimodel Ensemble System for Seasonal-to-Interannual Prediction (DEMETER) wind hindcasts. Forecasts obtained in this way are skillful during spring only, with highest skill during El Niño–Southern Oscillation years. During summer and fall, the DEMETER forecasts of wind anomalies limit the method’s ability to make reliable real predictions.
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13

Krapu, Gary L., Jan L. Eldridge, Cheri L. Gratto-Trevor, and Deborah A. Buhl. "Fat Dynamics of Arctic-Nesting Sandpipers During Spring in Mid-Continental North America." Auk 123, no. 2 (April 1, 2006): 323–34. http://dx.doi.org/10.1093/auk/123.2.323.

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Abstract We measured fresh body mass, total body fat, and fat-free dry mass (FFDM) of three species of Arctic-nesting calidrid sandpipers (Baird's Sandpiper [Calidris bairdii], hereafter “BASA”; Semipalmated Sandpiper [C. pusilla], hereafter “SESA”; and White-rumped Sandpiper [C. fuscicollis], hereafter “WRSA”) during spring stopovers in the Prairie Pothole Region (PPR) of North Dakota, and evaluated the contribution of stored fat to (1) energy requirements for migration to their Arctic-breeding grounds and (2) nutrient needs for reproduction. All spring migrant WRSA (n = 124) and BASA (n = 111), and all but 2 of 99 SESA we collected were ≥2 years old. Male and female BASA migrated through North Dakota concurrently, male SESA averaged earlier than females, and WRSA males preceded females. Fat indices (ratio of fat to FFDM) of male and female SESA and WRSA averaged approximately twice those of male and female BASA. Total body fat of male and female BASA increased with date in spring 1980, but not in 1981; slopes were similar for both sexes each year. Male and female SESA arrived lean in 1980 and 1981, and total body fat increased with date in both years, with similar slopes for all combinations of sex and year. Male and female WRSA arrived lean in 1980–1981 and 1981, respectively, and total body fat increased with date, whereas females arrived with fat reserves already acquired in 1980. Interspecific and sex differences in migration schedules probably contributed to variation in fat storage patterns by affecting maintenance energy costs and food availability. Estimated flight ranges of BASA suggest that few could have met their energy needs for migration to the breeding grounds exclusively from fat stored by the time of departure from North Dakota. Estimated flight ranges of SESA and WRSA, along with fresh body masses of both species when live-trapped on or near their breeding grounds in northern Canada, suggest that major parts of both populations stored adequate fat by departure from temperate mid-continental North America to meet their energy requirements for migration and part of their nutrient needs for reproduction. Dinámica de la Grasa en Chorlos que Nidifican en el Ártico durante la Primavera en el Área Continental Central de América del Norte
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14

Silva, Viviane B. S., and Ernesto H. Berbery. "Intense Rainfall Events Affecting the La Plata Basin." Journal of Hydrometeorology 7, no. 4 (August 1, 2006): 769–87. http://dx.doi.org/10.1175/jhm520.1.

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Abstract The circulation features associated with intense precipitation events over the La Plata Basin (LPB) during the austral summers of 2001/02 and 2002/03 are investigated using the Eta Model runs generated at the University of Maryland. Based on the main mode of variability over LPB, two regions were selected: (i) the region of Brazil that is at the core of the South American summer monsoon system (SAMS) and (ii) the central region of LPB in southeastern South America (SESA). First, a comparison between the 24-h total precipitation in the Eta Model and the 24-h observed precipitation was made. Results show that the Eta Model captures well the temporal variability of precipitation events in both regions, although a positive bias is noticed over SAMS. Likewise, the model reproduces the distribution of precipitation rate over SESA, but not over SAMS. Nevertheless, the distribution of the moisture flux convergence intensity, which represents the dynamical forcing, is closer in shape to the observed precipitation distribution, suggesting that the model can be a useful tool in identifying the forcing for heavy precipitation events over both regions. Composites of atmospheric and surface variables were constructed for intense precipitation events during austral summer over both regions. Intense rainfall over the central La Plata Basin (SESA) is linked to an amplified upper-tropospheric midlatitude wave pattern in which rainfall occurs just east of an enhanced cyclonic circulation. Accompanying this circulation pattern, an enhanced low-level jet (LLJ) transports warm, moist air from the Amazon toward the region, contributing to an increase in the thermal contrast over SESA. The combined patterns of thermal and dynamical variables suggest that large-scale systems, like frontal systems, are important in producing intense rainfall events. The SAMS region events have a similar upper-level structure as in SESA, but they are longer lived. In this case, the moisture fluxes are determined by an eastward shift of the LLJ, but also directly from the Amazon Basin to the north. As expected, precipitation events produce large increases of simulated runoff. The largest impact is on the SESA region, affecting the streamflow of the Paraná, Paraguay, and Uruguay, the three main rivers of the LPB.
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15

John, Ulrich, Ulfert Hapke, Hans-Jürgen Rumpf, and Anja Schumann. "Entwicklung und Testgüte der Skala zur Erfassung der Schwere der Alkoholabhängigkeit (SESA)." SUCHT 47, no. 6 (January 2001): 414–20. http://dx.doi.org/10.1024/suc.2001.47.6.414.

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Ziel der Arbeit ist die Darstellung von Entwicklung und Testgüte der »Skala zur Erfassung der Schwere der Alkoholabhängigkeit (SESA)« auf der Basis des Abhängigkeitssyndroms, das auch die Grundlage der Abhängigkeitsdiagnostik in den internationalen Krankheitsklassifikationssystemen ICD und DSM bildet. </P><P> Methodik: Die Testgüte wurde aufgrund von Analysen zur internen Konsistenz und dem Vergleich mit international verbreiteten diagnostischen Instrumenten in drei Stichproben bestimmt: 322 Alkoholabhängige in einer psychiatrischen Klinik, 226 Alkoholabhängige in einem Allgemeinkrankenhaus und 55 Alkoholabhängige aus einer repräsentativen Bevölkerungsuntersuchung. Die Ergebnisse weisen die SESA als intern konsistent und valide aus. Sie umfasst die Subskalen: Einengung des Trinkverhaltens, körperliche Entzugssymptome, Alkoholkonsum zur Vermeidung von Entzugssymptomen, psychische Entzugssymptome (Verlangen), Toleranzsteigerung, extreme Toleranzsteigerung sowie Toleranzumkehr. </P><P> Die Schlussfolgerungen zeigen, dass die SESA gegenüber den vergleichbaren internationalen Instrumenten ein optimiertes Verfahren zur Erfassung der Schwere der Alkoholabhängigkeit bildet. Die Validität ist durch ein besonders breites Spektrum unterschiedlicher Stichproben belegt.
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16

Bugnicourt, Jean-Marc, Bruno Bonnaire, Candice Picard, Aurélie Basille-Fantinato, and Olivier Godefroy. "Multiple reversible MRI abnormalities associated with SESA syndrome." Seizure 17, no. 8 (December 2008): 727–30. http://dx.doi.org/10.1016/j.seizure.2008.03.006.

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17

Santos, Eliete Correia dos. "Seminário de Saberes Arquivísticos (SESA): convergências e perspectivas." Archeion Online 5, no. 4 (December 30, 2017): 02. http://dx.doi.org/10.22478/ufpb.2318-6186.2017v5n4.37788.

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18

Ergüden, Bengü. "Dhh1 is a member of the SESA network." Yeast 36, no. 2 (November 11, 2018): 99–105. http://dx.doi.org/10.1002/yea.3363.

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19

Kuo, Ping-Chung, Zi-Han Kao, Shih-Wei Lee, and Sheng-Nan Wu. "Effects of Sesamin, the Major Furofuran Lignan of Sesame Oil, on the Amplitude and Gating of Voltage-Gated Na+ and K+ Currents." Molecules 25, no. 13 (July 4, 2020): 3062. http://dx.doi.org/10.3390/molecules25133062.

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Sesamin (SSM) and sesamolin (SesA) are the two major furofuran lignans of sesame oil and they have been previously noticed to exert various biological actions. However, their modulatory actions on different types of ionic currents in electrically excitable cells remain largely unresolved. The present experiments were undertaken to explore the possible perturbations of SSM and SesA on different types of ionic currents, e.g., voltage-gated Na+ currents (INa), erg-mediated K+ currents (IK(erg)), M-type K+ currents (IK(M)), delayed-rectifier K+ currents (IK(DR)) and hyperpolarization-activated cation currents (Ih) identified from pituitary tumor (GH3) cells. The exposure to SSM or SesA depressed the transient and late components of INa with different potencies. The IC50 value of SSM needed to lessen the peak or sustained INa was calculated to be 7.2 or 0.6 μM, while that of SesA was 9.8 or 2.5 μM, respectively. The dissociation constant of SSM-perturbed inhibition on INa, based on the first-order reaction scheme, was measured to be 0.93 μM, a value very similar to the IC50 for its depressant action on sustained INa. The addition of SSM was also effective at suppressing the amplitude of resurgent INa. The addition of SSM could concentration-dependently inhibit the IK(M) amplitude with an IC50 value of 4.8 μM. SSM at a concentration of 30 μM could suppress the amplitude of IK(erg), while at 10 μM, it mildly decreased the IK(DR) amplitude. However, the addition of neither SSM (10 μM) nor SesA (10 μM) altered the amplitude or kinetics of Ih in response to long-lasting hyperpolarization. Additionally, in this study, a modified Markovian model designed for SCN8A-encoded (or NaV1.6) channels was implemented to evaluate the plausible modifications of SSM on the gating kinetics of NaV channels. The model demonstrated herein was well suited to predict that the SSM-mediated decrease in peak INa, followed by increased current inactivation, which could largely account for its favorable decrease in the probability of the open-blocked over open state of NaV channels. Collectively, our study provides evidence that highlights the notion that SSM or SesA could block multiple ion currents, such as INa and IK(M), and suggests that these actions are potentially important and may participate in the functional activities of various electrically excitable cells in vivo.
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20

Zhang, Honghai, Thomas L. Delworth, Fanrong Zeng, Gabriel Vecchi, Karen Paffendorf, and Liwei Jia. "Detection, Attribution, and Projection of Regional Rainfall Changes on (Multi-) Decadal Time Scales: A Focus on Southeastern South America." Journal of Climate 29, no. 23 (November 11, 2016): 8515–34. http://dx.doi.org/10.1175/jcli-d-16-0287.1.

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Abstract Observed austral summertime (November through April) rainfall in southeastern South America (SESA)—including northern Argentina, Uruguay, southern Brazil, and Paraguay—has exhibited substantial low-frequency variations with a multidecadal moistening trend during the twentieth century and a subsequent decadal drying trend during the current century. Understanding the mechanisms responsible for these variations is essential for predicting long-term rainfall changes. Here with a suite of attribution experiments using a pair of high-resolution global climate models, GFDL CM2.5 and FLOR-FA, the authors investigate the causes of these regional rainfall variations. Both models reproduce the twentieth-century moistening trend, albeit with a weaker magnitude than observed, in response to the radiative forcing associated with increasing greenhouse gases. The increasing greenhouse gases drive tropical expansion; consequently, the subtropical dry branch of Hadley cell moves away from SESA, leading to the rainfall increase. The amplitude discrepancy between the observed and simulated rainfall changes suggests a possible underestimation by the models of the atmospheric response to the radiative forcing, as well as an important role for low-frequency internal variability in the observed moistening trend. Over the current century, increasing greenhouse gases drive a continuous SESA rainfall increase in the models. However, the observed decadal rainfall decline is largely (~60%) reproduced in response to the observed Pacific trade wind strengthening, which is likely associated with natural Pacific decadal variability. These results suggest that the recent summertime rainfall decline in SESA is temporary and that the positive trend will resume in response to both increasing greenhouse gases and a return of Pacific trade winds to normal conditions.
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21

Enomoto, Gen, Ni-Ni-Win, Rei Narikawa, and Masahiko Ikeuchi. "Three cyanobacteriochromes work together to form a light color-sensitive input system for c-di-GMP signaling of cell aggregation." Proceedings of the National Academy of Sciences 112, no. 26 (June 15, 2015): 8082–87. http://dx.doi.org/10.1073/pnas.1504228112.

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Cyanobacteriochromes (CBCRs) are cyanobacterial photoreceptors that have diverse spectral properties and domain compositions. Although large numbers of CBCR genes exist in cyanobacterial genomes, no studies have assessed whether multiple CBCRs work together. We recently showed that the diguanylate cyclase (DGC) activity of the CBCR SesA from Thermosynechococcus elongatus is activated by blue-light irradiation and that, when irradiated, SesA, via its product cyclic dimeric GMP (c-di-GMP), induces aggregation of Thermosynechococcus vulcanus cells at a temperature that is suboptimum for single-cell viability. For this report, we first characterize the photobiochemical properties of two additional CBCRs, SesB and SesC. Blue/teal light-responsive SesB has only c-di-GMP phosphodiesterase (PDE) activity, which is up-regulated by teal light and GTP. Blue/green light-responsive SesC has DGC and PDE activities. Its DGC activity is enhanced by blue light, whereas its PDE activity is enhanced by green light. A ΔsesB mutant cannot suppress cell aggregation under teal-green light. A ΔsesC mutant shows a less sensitive cell-aggregation response to ambient light. ΔsesA/ΔsesB/ΔsesC shows partial cell aggregation, which is accompanied by the loss of color dependency, implying that a nonphotoresponsive DGC(s) producing c-di-GMP can also induce the aggregation. The results suggest that SesB enhances the light color dependency of cell aggregation by degrading c-di-GMP, is particularly effective under teal light, and, therefore, seems to counteract the induction of cell aggregation by SesA. In addition, SesC seems to improve signaling specificity as an auxiliary backup to SesA/SesB activities. The coordinated action of these three CBCRs highlights why so many different CBCRs exist.
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Rothmeier, J., M. Friese, F. Willemsen, and W. Froescher. "Subacute Encephalopathy with Seizures in Chronic Alcoholism (SESA Syndrome)." Clinical Electroencephalography 32, no. 4 (October 2001): 186–90. http://dx.doi.org/10.1177/155005940103200405.

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Fernández-Torre, José L., and Peter W. Kaplan. "Subacute encephalopathy with seizures in alcoholics (SESA syndrome) revisited." Seizure 23, no. 5 (May 2014): 393–96. http://dx.doi.org/10.1016/j.seizure.2014.02.002.

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24

Levin, M., T. Dolan, and C. E. Taylor. "SEM HISTORY: THOMAS J. DOLAN SESA PRESIDENT 1951–52." Experimental Techniques 24, no. 5 (September 2000): 10–12. http://dx.doi.org/10.1111/j.1747-1567.2000.tb02349.x.

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25

Vogt, Bjoern, Gregor Toporowski, Georg Gosheger, Jan Duedal Rölfing, Dieter Rosenbaum, Frank Schiedel, Andrea Laufer, et al. "Subtalar Arthroereisis for Flexible Flatfoot in Children—Clinical, Radiographic and Pedobarographic Outcome Comparing Three Different Methods." Children 8, no. 5 (April 30, 2021): 359. http://dx.doi.org/10.3390/children8050359.

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Subtalar arthroereises (STA) is a minimally invasive and reversible surgery to correct symptomatic flexible flatfoot (FFF) in children. Various techniques were described either applying expandable sinus tarsi implants or lateral calcaneus stop screws. Studies comparing the outcome of STA with different devices are rare. This retrospective single-center cohort study analyzes the results of STA using three different implants. 113 STA were performed in 73 consecutive patients (28 females). Mean age at surgery was 10.8 years (range 5–16). Mean follow-up was 29.0 months (range 1–111). In 21 feet the non-absorbable Kalix® endorthesis and in 56 feet the absorbable Giannini endorthesis were applied. Subtalar extraarticular screw arthroereises (SESA) was conducted in 36 feet. Clinical, radiographic and pedobarographic parameters were analyzed. No intraoperative complications were observed. All three procedures achieved comparable improvements of the clinical, radiographic and pedobarographic parameters. The mean foot function index (FFI) improved from 36.4 (range 12–63) to 22.8 (range 2–55). The mean preoperative calcaneal inclination angle and the lateral talocalcaneal angle improved from 9.5° (range 0–22) and 42.3° (range 21–62) to 12.8° (range 0–26) and 37.6° (range 15–56), respectively. Pedobarographically determined values of the arch index, the medial midfoot contact area and the medial forefoot peak pressure decreased. In contrast to SESA (1/36, 3%), a higher incidence of implant-related complications was observed using Kalix® (6/21, 29%) and Giannini (10/56, 8%) sinus tarsi implants. Peroneal muscle contractures only occurred in the SESA group (4/36, 11%). Premature removal due to treatment-related complications was necessary in 6/21 Kalix® implants (29%), 4/56 Giannini implants (7%) and 4/36 SESA implants (11%). Implant choice for treatment of painful FFF in children with STA seems to play a subordinate role. Clinical, radiographic and pedobarographic outcomes are comparable between the applied implants. Surgeons and patients should be aware of the different spectrum of implant-related complications. Treatment can be reliably monitored by radiation-free pedobarography providing dynamic information about the deformity.
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26

Ergüden, Bengü. "Pom34 mRNA is the Only Target of the Sesa Network." Hacettepe Journal of Biology and Chemistry 4, no. 45 (December 25, 2017): 539–45. http://dx.doi.org/10.15671/hjbc.2018.195.

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27

Otto, Franz G., and Ralf Kozian. "Subacute Encephalopathy with Epileptic Seizures in Alcoholism (SESA): Case Report." Clinical Electroencephalography 32, no. 4 (October 2001): 184–85. http://dx.doi.org/10.1177/155005940103200404.

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28

Cancelada, Maite, Paola Salio, Daniel Vila, Stephen W. Nesbitt, and Luciano Vidal. "Backward Adaptive Brightness Temperature Threshold Technique (BAB3T): A Methodology to Determine Extreme Convective Initiation Regions Using Satellite Infrared Imagery." Remote Sensing 12, no. 2 (January 20, 2020): 337. http://dx.doi.org/10.3390/rs12020337.

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Thunderstorms in southeastern South America (SESA) stand out in satellite observations as being among the strongest on Earth in terms of satellite-based convective proxies, such as lightning flash rate per storm, the prevalence for extremely tall, wide convective cores and broad stratiform regions. Accurately quantifying when and where strong convection is initiated presents great interest in operational forecasting and convective system process studies due to the relationship between convective storms and severe weather phenomena. This paper generates a novel methodology to determine convective initiation (CI) signatures associated with extreme convective systems, including extreme events. Based on the well-established area-overlapping technique, an adaptive brightness temperature threshold for identification and backward tracking with infrared data is introduced in order to better identify areas of deep convection associated with and embedded within larger cloud clusters. This is particularly important over SESA because ground-based weather radar observations are currently limited to particular areas. Extreme rain precipitation features (ERPFs) from Tropical Rainfall Measurement Mission are examined to quantify the full satellite-observed life cycle of extreme convective events, although this technique allows examination of other intense convection proxies such as the identification of overshooting tops. CI annual and diurnal cycles are analyzed and distinctive behaviors are observed for different regions over SESA. It is found that near principal mountain barriers, a bimodal diurnal CI distribution is observed denoting the existence of multiple CI triggers, while convective initiation over flat terrain has a maximum frequency in the afternoon.
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Strackx, Raoul, Pieter Agten, Niels Avonds, and Frank Piessens. "Salus: Kernel Support for Secure Process Compartments." ICST Transactions on Security and Safety 2, no. 3 (January 30, 2015): e1. http://dx.doi.org/10.4108/sesa.2.3.e1.

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30

Elashry, I., Y. Mu, and W. Susilo. "Mediated Encryption: Analysis and Design." ICST Transactions on Security and Safety 2, no. 3 (January 30, 2015): e2. http://dx.doi.org/10.4108/sesa.2.3.e2.

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31

Ahmat, Daouda, Damien Magoni, and Tegawendé F. Bissyandé. "End-to-End Key Exchange through Disjoint Paths in P2P Networks." ICST Transactions on Security and Safety 2, no. 3 (January 30, 2015): e3. http://dx.doi.org/10.4108/sesa.2.3.e3.

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32

Fan, Xinxin, Kalikinkar Mandal, and Guang Gong. "WG-8: A Lightweight Stream Cipher for Resource-Constrained Smart Devices." ICST Transactions on Security and Safety 2, no. 3 (January 30, 2015): e4. http://dx.doi.org/10.4108/sesa.2.3.e4.

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Maglaras, Leandros A., and Jianmin Jiang. "A novel intrusion detection method based on OCSVM and K-means recursive clustering." ICST Transactions on Security and Safety 2, no. 3 (January 30, 2015): e5. http://dx.doi.org/10.4108/sesa.2.3.e5.

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34

Enomoto, Gen, Ryouhei Nomura, Takashi Shimada, Ni-Ni-Win, Rei Narikawa, and Masahiko Ikeuchi. "Cyanobacteriochrome SesA Is a Diguanylate Cyclase That Induces Cell Aggregation inThermosynechococcus." Journal of Biological Chemistry 289, no. 36 (July 24, 2014): 24801–9. http://dx.doi.org/10.1074/jbc.m114.583674.

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35

Fernández-Torre, José L., Zaloa Aguirre-Arrizubieta, Francisco Casariego Pola, and Andrés González-Mandly. "Sesa syndrome: A subtype of localisation-related non-convulsive status epilepticus?" Seizure 18, no. 4 (May 2009): 306–7. http://dx.doi.org/10.1016/j.seizure.2008.11.007.

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36

Drake-Pérez, Marta, Enrique Marco de Lucas, John Lyo, and José L. Fernández-Torre. "Neuroimaging features in subacute encephalopathy with seizures in alcoholics (SESA syndrome)." Seizure 40 (August 2016): 102–7. http://dx.doi.org/10.1016/j.seizure.2016.06.009.

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37

Gelbrecht, Maximilian, Niklas Boers, and Jürgen Kurths. "Phase coherence between precipitation in South America and Rossby waves." Science Advances 4, no. 12 (December 2018): eaau3191. http://dx.doi.org/10.1126/sciadv.aau3191.

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The dominant mode of intraseasonal precipitation variability during the South American monsoon is the so-called precipitation dipole between the South Atlantic convergence zone (SACZ) and southeastern South America (SESA). It affects highly populated areas that are of substantial importance for the regional food supplies. Previous studies using principal components analysis or complex networks were able to describe and characterize this variability pattern, but crucial questions regarding the responsible physical mechanism remain open. Here, we use phase synchronization techniques to study the relation between precipitation in the SACZ and SESA on the one hand and southern hemisphere Rossby wave trains on the other hand. In combination with a conceptual model, this approach demonstrates that the dipolar precipitation pattern is caused by the southern hemisphere Rossby waves. Our results thus show that Rossby waves are the main driver of the monsoon season variability in South America, a finding that has important implications for synoptic-scale weather forecasts.
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38

Kuswardani, Kuswardani, Didik Purnomo, and Suci Amanati. "Pengaruh Nebulizer, Infra Red dan Chest Therapy terhadap Asma Bronchiale." Jurnal Fisioterapi dan Rehabilitasi 1, no. 1 (January 9, 2017): 49–56. http://dx.doi.org/10.33660/jfrwhs.v1i1.10.

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Asma Bronchial adalah penyakit inflamasi obstruktif yang ditandai oleh periode episodik spasme otot-otot polos dalam dinding saluran udara bronchial (spasme bronkus). Spasmebronkus itu menyempitkan jalan nafas, sehingga membuat pernafasan menjadi sulit dan menimbulkan bunyi mengi. Tahun 2006, jumlah penderita asma diperkirakan mencapai 300 juta orang di dunia, angka ini diperkirakan akan terus meningkat 400 juta orang pada 2025. Rumusan masalah dalam penelitian ini adalah bagaimana pengaruh nebulizer, infra red dan chest therapy terhadap penderita asma bronchial. Populasi penelitian ini adalah pasien penderita asma bronchiale. Sampel penelitian ini menggunakan seluruh populasi, yaitu sebanyak 8 pasien yang secara keseluruhan diambil sebagai sampel penelitian. Pengumpulan data didapat dari pemeriksaan Sesak Napas dengan skala borg. Skala Borg sebagai pemeriksaan sesak nafas. Hasil uji t menunjukkan Sig. = 0,000 (<0,05), maka Ho ditolak dan Ha diterima. Hal ini berarti sesa nafas sesudah dan sebelum tindakan nebulizer, infra red dan chest therapy tidak sama. Berdasarkan hasil analisis data dan pembahasan maka dapat disimpulkan bahwa Nebulizer, infra red dan Chest Therapy dapat mengurangi sesak nafas pada penderita asma bronchial.
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39

Ruiz, Juan J., Celeste Saulo, and Julia Nogués-Paegle. "WRF Model Sensitivity to Choice of Parameterization over South America: Validation against Surface Variables." Monthly Weather Review 138, no. 8 (August 1, 2010): 3342–55. http://dx.doi.org/10.1175/2010mwr3358.1.

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Abstract The Weather and Research Forecast model is tested over South America in different configurations to identify the one that gives the best estimates of observed surface variables. Systematic, nonsystematic, and total errors are computed for 48-h forecasts initialized with the NCEP Global Data Assimilation System (GDAS). There is no unique model design that best fits all variables over the whole domain, and nonsystematic errors for all configurations differ little from one another; such differences are in most cases smaller than the observed day-to-day variability. An ensemble mean consisting of runs with different parameterizations gives the best skill for the whole domain. Surface variables are highly sensitive to the choice of land surface models. Surface temperature is well represented by the Noah land model, but dewpoint temperature is best estimated by the simplest land surface model considered here, which specifies soil moisture based on climatology. This underlines the need for better understanding of humid processes at the subgrid scale. Surface wind errors decrease the intensity of the low-level jet, reducing expected heat and moisture advection over southeast South America (SESA), with negative precipitation errors over SESA and positive biases over the South Atlantic convergence zone (SACZ). This pattern of errors suggests feedbacks between wind errors, precipitation, and surface processes as follows: an increase of precipitation over the SACZ produces compensating descent in SESA, with more stable stratification, less rain, less soil moisture, and decreased rain. This is a clear example of how local errors are related to regional circulation, and suggests that improvement of model performance requires not only better parameterizations at the subgrid scales, but also improved regional models.
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40

Crosta, G. B. "Failure and flow development of a complex slide: the 1993 Sesa landslide." Engineering Geology 59, no. 1-2 (January 2001): 173–99. http://dx.doi.org/10.1016/s0013-7952(00)00073-9.

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41

Choi, Jun Yong, Jiwon Kwon, and Eun-Kee Bae. "A pathophysiologic approach for subacute encephalopathy with seizures in alcoholics (SESA) syndrome." Journal of Clinical Neuroscience 21, no. 9 (September 2014): 1649–52. http://dx.doi.org/10.1016/j.jocn.2013.11.045.

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42

Ciesielski, Paul E., and Richard H. Johnson. "Contrasting Characteristics of Convection over the Northern and Southern South China Sea during SCSMEX." Monthly Weather Review 134, no. 4 (April 1, 2006): 1041–62. http://dx.doi.org/10.1175/mwr3113.1.

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Abstract Observations from two enhanced sounding arrays during the May–June 1998 South China Sea Monsoon Experiment (SCSMEX) are used to determine and contrast the properties of convection over the northern and southern South China Sea (SCS). A regression analysis between SST data and monthly rainfall indicates that the ENSO signal exerted a strong influence on the rainfall distribution over the SCS during SCSMEX. This resulted in wetter-than-normal conditions along the south China coast and northern SCS, and generally drier-than-average conditions elsewhere, particularly over the Philippine Islands. The monsoon onset as determined by a shift in the low-level winds from easterly to southwesterly over the SCS occurred around mid-May. Over the southern enhanced sounding array (SESA), the onset was characterized by a rainy period associated with the passage of a convectively coupled Kelvin wave. This was followed by a weeklong break and then several episodic rain events with increasingly higher rain rates. Rainfall over the northern enhanced sounding array (NESA), which was largely out of phase with SESA rainfall events, occurred primarily during two 10-day periods separated by a weeklong break. Convective characteristics over the SESA, deduced primarily from heat and moisture budget profiles, indicate a high stratiform rain fraction consisting of alternating periods with decaying mesoscale systems that organized near the western Borneo coastline and shallower convective clouds. In contrast, NESA-averaged profiles were indicative of deep convection with a relatively small stratiform rain fraction, which was confirmed with radar analyses during the onset convective period. The diurnal cycle of convection is a dominant feature throughout much of the SCS. Over both budget regions, early morning (0500–0800 LT) convective systems were frequently initiated near the coasts, then gradually dissipated during the course of the day as the midlevel steering currents moved the systems away from the coastline. These decaying convective systems resulted in an early afternoon (1400 LT) rainfall peak over both sonde arrays.
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43

"SESA Annual Report, 1982-83." Experimental Techniques 7, no. 7 (January 28, 2008): 30–32. http://dx.doi.org/10.1111/j.1747-1567.1983.tb01787.x.

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44

"President Ligon's Outlook on SESA." Experimental Techniques 7, no. 7 (January 28, 2008): 34–35. http://dx.doi.org/10.1111/j.1747-1567.1983.tb01788.x.

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45

"Proceedings—1983 SESA Fall Meeting." Experimental Techniques 9, no. 1 (January 1985): 42. http://dx.doi.org/10.1111/j.1747-1567.1985.tb01965.x.

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46

Varuolo-Clarke, Arianna M., Jason E. Smerdon, A. Park Williams, and Richard Seager. "Gross discrepancies between observed and simulated 20th-21st-century precipitation trends in Southeastern South America." Journal of Climate, May 17, 2021, 1–44. http://dx.doi.org/10.1175/jcli-d-20-0746.1.

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AbstractSoutheastern South America (SESA; encompassing Paraguay, Southern Brazil, Uruguay, and northern Argentina) experienced a 27% increase in austral summer precipitation from 1902-2019, one of the largest observed trends in seasonal precipitation globally. Previous research identifies Atlantic Multidecadal Variability and anthropogenic forcing from stratospheric ozone depletion and greenhouse gas emissions as key factors contributing to the positive precipitation trends in SESA. We analyze multi-model ensemble simulations from Phases 5 and 6 of the Coupled Model Intercomparison Project (CMIP) and find that not only do Earth System Models simulate positive SESA precipitation trends that are much weaker over the historical interval, but some models persistently simulate negative SESA precipitation trends under historical forcings. Similarly, 16-member ensembles from two atmospheric models forced with observed historical sea surface temperatures never simulate precipitation trends that even reach the lower bound of the observed trend’s range of uncertainty. Moreover, while future 21st-century projections from CMIP6 yield positive ensemble mean precipitation trends over SESA that grow with increasing greenhouse-gas emissions, the mean forced response never exceeds the observed historical trend. Pre-industrial control runs from CMIP6 indicate that some models do occasionally simulate centennial-scale trends in SESA that fall within the observational range, but most models do not. Results point to significant uncertainties in the attribution of anthropogenically forced influences on the observed increases in precipitation over SESA, while also suggesting that internal decadal-to-centennial variability of unknown origin and not present in state-of-the-art models may have also played a large role in generating the 20th-21st-century SESA precipitation trend.
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Hu, Xinjia, Jan Eichner, Daoyi Gong, Marcelo Barreiro, and Holger Kantz. "Combined impact of ENSO and Antarctic Oscillation on austral spring precipitation in Southeastern South America (SESA)." Climate Dynamics, November 19, 2022. http://dx.doi.org/10.1007/s00382-022-06592-8.

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AbstractSoutheastern South America (SESA)’s precipitation is thought to be influenced by both El Niño Southern Oscillation (ENSO) and Antarctic Oscillation (AAO), especially in austral spring. Previous studies conclude AAO can modulate ENSO’s impact on precipitation over the SESA region without differentiating between El Niño and La Niña events. In the present study, we use composite analysis to further explore the combined impact of AAO and ENSO on austral spring precipitation over Southeastern South America (SESA) to answer this question and explain the dynamic mechanisms. We found that different AAO phases can influence La Niña’s impact on SESA austral spring precipitation considerably, while this does not apply for El Niño events. From our analysis, we found that AAO exerts more impact on austral spring precipitation over SESA compared to ENSO during La Niña years by influencing northerly wind and southward water vapor flux, which contributes most of the moisture into the SESA region, due to the strengthening of South Atlantic subtropical anticyclone and stronger meridional gradient in low-level pressure. Besides, there is an upper-level trough (ridge) over subtropical South America indicating advection of cyclonic (anticyclonic) vorticity inducing anomalous increase (decrease) of precipitation over that region during La Niña/AAO− (La Niña/AAO+). We do not see this opposite difference within El Niño groups combined with different phases of AAO.
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GÜNDOĞDU, Tevfik Mert, Erkan ERKMEN, and Öykü ÖZTÜRK GÜNDOĞDU. "DENTAL İMPLANTOLOJİDE SONLU ELEMANLAR STRES ANALİZİ YÖNTEMİ İLE YAPILABİLEN DEĞERLENDİRMELER." ADO Klinik Bilimler Dergisi, June 6, 2022. http://dx.doi.org/10.54617/adoklinikbilimler.1094962.

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Günümüzde eksik dişlerin dental implantlar ile tedavi edilmesi rutin bir işlem haline gelmiştir. Dental implantların biyomekanik özellikleri, oklüzal yüklerin stres dağılımını değiştirerek dental implantların klinik başarısını etkilemektedir. İmplant kayıplarının ve komplikasyonların önlenmesi amacıyla oluşabilecek biyomekanik etkilerin önceden kavranması önem taşımaktadır. Dental implantlar çevresindeki yüklerin dağılımı ile ilgili yapılan çalışmalarda, yüklerin homojen dağıtıldığı durumlarda periimplant marjinal kemik kaybının daha az olduğu belirtilmiştir. Bahsedilen biyomekanik etkilerin in vitro ortamda belirlenmesi amacıyla dental implantoloji alanında sonlu elemanlar stres analizi yöntemi (SESA) yöntemi kullanılmaktadır. Bu çalışmada SESA yönteminin dental implantoloji alanında kullanımını araştıran mevcut literatür özetlenmiştir. Bu sayede SESA yöntemi ile implant kayıplarının ve komplikasyonların önlenmesi amacıyla in vitro ortamda elde edilen bilgilerin klinik başarıdaki rolünü arttırmak amaçlanmaktadır.
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Medrano, Leonardo Adrián, Mercedes Fernández Liporace, and Edgardo Pérez. "Sistema de Evaluación Informatizado de la Satisfacción Académica para Estudiantes Universitarios de Primer Año." Electronic Journal of Research in Education Psychology 12, no. 33 (November 30, 2017). http://dx.doi.org/10.25115/ejrep.33.13131.

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Introducción. Los test informatizados se han transformado en uno de los métodos de evaluación educativa de mayor uso y eficiencia. En el ámbito de la evaluación psicoeducativa, cabe destacar los esfuerzos para generar sistemas de evaluación informatizados que permitan identificar alumnos en riesgo de abandonar sus estudios. Atendiendo a la importancia de la satisfacción académica en la permanencia académica, el presente trabajo tuvo por objetivo des-arrollar un Sistema de Evaluación Informatizado de la Satisfacción Académica (SESA).Método. El SESA evalúa diferentes variables implicadas en el modelo social cognitivo de satisfacción académica, tales como autoeficacia académica, expectativas de resultados, progreso en metas académicas y satisfacción académica. Se describe el proceso de informatización del SESA atendiendo a las directrices propuestas por la Comisión Internacional de Test y resultados psicométricos sobre la estructura factorial y consistencia interna del mismo (N=377).Resultados. En términos generales los resultados obtenidos fueron satisfactorios y no se observaron dificultades o limitaciones que pudieran obstaculizar el futuro desarrollo del sistema. En relación al proceso de informatización del SESA-U se cumplimentaron de manera adecuada los estándares de tecnología, calidad, control y seguridad propuestos por la ITC. La estructura interna de todas las escalas fue teóricamente interpretable y semejante a la reportada en los trabajos originales.Discusión y Conclusiones. Restan por desarrollar nuevos estudios tendientes a aportar mayores evidencias de validez. El SESA-U constituye un sistema adecuado para detectar de manera temprana estudiantes de primer año en riesgo de abandonar sus estudios.
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50

"THOMAS J. DOLAN SESA PRESIDENT 1951–52." Experimental Techniques 24, no. 2 (March 2000): 10. http://dx.doi.org/10.1111/j.1747-1567.2000.tb02261.x.

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