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Zeitschriftenartikel zum Thema „And the East“

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Autor: Grafiati

Veröffentlicht am 25. Juli 2024

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1

Liu, Jiawei, Haiming Xu und Jiechun Deng. „Projections of East Asian summer monsoon change at global warming of 1.5 and 2 °C“. Earth System Dynamics 9, Nr. 2 (27.04.2018): 427–39. http://dx.doi.org/10.5194/esd-9-427-2018.

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Abstract. Much research is needed regarding the two long-term warming targets of the 2015 Paris Agreement, i.e., 1.5 and 2 ∘C above pre-industrial levels, especially from a regional perspective. The East Asian summer monsoon (EASM) intensity change and associated precipitation change under both warming targets are explored in this study. The multimodel ensemble mean projections by 19 CMIP5 models show small increases in EASM intensity and general increases in summer precipitation at 1.5 and 2 ∘C warming, but with large multimodel standard deviations. Thus, a novel multimodel ensemble pattern regression (EPR) method is applied to give more reliable projections based on the concept of emergent constraints, which is effective at tightening the range of multimodel diversity and harmonize the changes of different variables over the EASM region. Future changes projected by using the EPR method suggest decreased precipitation over the Meiyu belt and increased precipitation over the high latitudes of East Asia and Central China, together with a considerable weakening of EASM intensity. Furthermore, reduced precipitation appears over 30–40∘ N of East Asia in June and over the Meiyu belt in July, with enhanced precipitation at their north and south sides. These changes in early summer are attributed to a southeastward retreat of the western North Pacific subtropical high (WNPSH) and a southward shift of the East Asian subtropical jet (EASJ), which weaken the moisture transport via southerly wind at low levels and alter vertical motions over the EASM region. In August, precipitation would increase over the high latitudes of East Asia with more moisture from the wetter area over the ocean in the east and decrease over Japan with westward extension of WNPSH. These monthly precipitation changes would finally contribute to a tripolar pattern of EASM precipitation change at 1.5 and 2 ∘C warming. Corrected EASM intensity exhibits a slight difference between 1.5 and 2 ∘C, but a pronounced moisture increase during extra 0.5 ∘C leads to enhanced EASM precipitation over large areas in East Asia at 2 ∘C warming.

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2

Parker, Stephen. „East is East“. IFLA Journal 32, Nr. 2 (Juni 2006): 91–92. http://dx.doi.org/10.1177/0340035206066404.

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3

Cheng, Wendy. „East of East“. Boom 5, Nr. 1 (2015): 20–28. http://dx.doi.org/10.1525/boom.2015.5.1.20.

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While Los Angeles’s San Gabriel Valley is best known for being the “first suburban Chinatown,” it is actually a lively, multiethnic, and multiracial community with a complex past, and an emerging arts scene that celebrates that complexity. Today, the “SGV” constitutes the largest, majority-Asian American and Latino community in the United States. Its social and cultural mix make it a vibrant example of suburban cosmopolitanism, in which diverse residents live in relative harmony, with mutual respect for difference. Local groups such as the South El Monte Arts Posse have begun to make work that reflects this ethos, and could reshape normative ideas of what it means to be American.

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Jászay, Tamás. „East is East?“ Theatron 16, Nr. 4 (2022): 165–69. http://dx.doi.org/10.55502/the.2022.4.165.

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The volume focuses on directors who began their careers mainly around the time of the regime changes in Eastern Europe, and presents the careers of twenty theatre directors who have had a decisive influence on the theatrical landscape of their countries, regions, and the European continent in the past decades. Chapters of similar length and structure review the years of education and the early steps, then report on national and international successes, and the milestones of their careers. The essays summarise in headings the artistic credo of the directors, the most important features of their aesthetics, placing their work in historical, social, and artistic context.

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5

Scott, Hilda, und Tanya Renne. „When East Meets East“. Women's Review of Books 14, Nr. 8 (Mai 1997): 18. http://dx.doi.org/10.2307/4022696.

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6

Lee, Se Woong. „Circulating East to East“. Journal of Studies in International Education 21, Nr. 2 (16.03.2017): 170–90. http://dx.doi.org/10.1177/1028315317697540.

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Every year, substantial numbers of students choose to study abroad, and China is one of the largest exporters of international students. Interestingly, instead of choosing English-speaking countries, increasingly more Chinese students are choosing nearby Asian countries as their destination to study abroad, particularly Korea. Despite this emerging trend, little is known regarding why Chinese students have begun to choose Korea and its universities or their level of educational satisfaction with their study-abroad choices. Extrapolating from the push–pull model, this study utilized a combination of quantitative and qualitative research methods to examine factors affecting students’ choice to study in Korea. Notably, this study concluded that although low institution selectivity is a strong pull factor, that selectivity is also a determinant of students’ study-abroad satisfaction. This study contributes to the limited research by exploring the distinct push–pull factors of Chinese students who are studying in Asia—East to East—particularly in Korea.

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7

Gibler, Douglas M. „East or Further East?“ Journal of Peace Research 36, Nr. 6 (November 1999): 627–37. http://dx.doi.org/10.1177/0022343399036006002.

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8

Roberts, Mervin F. „East Is East and …“. Fisheries 37, Nr. 10 (11.10.2012): 464–65. http://dx.doi.org/10.1080/03632415.2012.722879.

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9

Rajan, T. V. „East is East, etc.“ Cancer Biology & Therapy 1, Nr. 3 (05.05.2002): 313–14. http://dx.doi.org/10.4161/cbt.88.

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10

Wang, Zhili, Lei Lin, Meilin Yang, Yangyang Xu und Jiangnan Li. „Disentangling fast and slow responses of the East Asian summer monsoon to reflecting and absorbing aerosol forcings“. Atmospheric Chemistry and Physics 17, Nr. 18 (19.09.2017): 11075–88. http://dx.doi.org/10.5194/acp-17-11075-2017.

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Abstract. We examine the roles of fast and slow responses in shaping the total equilibrium response of the East Asian summer monsoon (EASM) to reflecting (sulfate, SO4) and absorbing (black carbon, BC) aerosol forcings over the industrial era using the Community Earth System Model version 1 (CESM1). Our results show that there is a clear distinction between fast and slow responses of the EASM to aerosol forcings and the slow climate response due to aerosol-induced change in sea surface temperature (SST) plays an important role in the impacts of aerosols on the EASM. The EASM is weakened by a decrease in land–sea surface thermal contrast in the fast response (FR) component to SO4 forcing, whereas the weakening is more intensive due to the changes in tropospheric thermodynamic and dynamic structures in the slow response (SR) component to SO4. The total climate adjustment caused by SO4 is a significant weakening of the EASM and a decrease in precipitation. The BC-induced fast adjustment strengthens the EASM both by increasing the local land–sea surface thermal contrast and shifting the East Asian subtropical jet (EASJ) northwards. The BC-induced slow climate adjustment, however, weakens the EASM through altering the atmospheric temperature and circulation. Consequently, the EASM is slightly enhanced, especially north of 30° N, in the total response (TR) to BC. The spatial patterns of precipitation change over East Asia due to BC are similar in the total response and slow response. This study highlights the importance of ocean response to aerosol forcings in driving the changes of the EASM.

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Li, Fuxing, Dong Chen, Qiuhong Tang, Wenhong Li und Xuejun Zhang. „Hydrological Response of East China to the Variation of East Asian Summer Monsoon“. Advances in Meteorology 2016 (2016): 1–12. http://dx.doi.org/10.1155/2016/4038703.

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The sensitivity of hydrologic variables in East China, that is, runoff, precipitation, evapotranspiration, and soil moisture to the fluctuation of East Asian summer monsoon (EASM), is evaluated by the Mann-Kendall correlation analysis on a spatial resolution of 1/4° in the period of 1952–2012. The results indicate remarkable spatial disparities in the correlation between the hydrologic variables and EASM. The regions in East China susceptible to hydrological change due to EASM fluctuation are identified. When the standardized anomaly of intensity index of EASM (EASMI) is above 1.00, the runoff of Haihe basin has increased by 49% on average, especially in the suburb of Beijing and Hebei province where the runoff has increased up to 105%. In contrast, the runoff in the basins of Haihe and Yellow River has decreased by about 27% and 17%, respectively, when the standardized anomaly of EASMI is below −1.00, which has brought severe drought to the areas since mid-1970s. The study can be beneficial for national or watershed agencies developing adaptive water management strategies in the face of global climate change.

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12

Chen, Haishan, Fangda Teng, Wanxin Zhang und Hong Liao. „Impacts of Anomalous Midlatitude Cyclone Activity over East Asia during Summer on the Decadal Mode of East Asian Summer Monsoon and Its Possible Mechanism“. Journal of Climate 30, Nr. 2 (Januar 2017): 739–53. http://dx.doi.org/10.1175/jcli-d-16-0155.1.

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By using an objective identification and tracking algorithm of the cyclone, the statistics of midlatitude cyclone activity in East Asia during summer for the period 1979–2013 were analyzed. The impact of the midlatitude summer cyclone anomalies in East Asia on the decadal mode of East Asian summer monsoon (EASM) was investigated and possible mechanisms were proposed. The possible reasons for the anomalous cyclone activity from the perspective of land surface thermal forcing were also explored. Results indicate that the midlatitude summer cyclone activity over East Asia exhibits decadal changes in the period of 1979–2013 and is significantly weakened after early 1990s. Further analysis indicates that there is a close relationship between the midlatitude summer cyclone activity over East Asia and the decadal variation of EASM; when the midlatitude summer cyclone activity over East Asia is strong (weak), EASM tends to be intensified (weakened), and the weak cyclone activity after 1993 generally coincides with the decadal weakening of EASM. Moreover, there is a close linkage between the weakening of cyclonic activity after the early 1990s and the nonuniform surface warming of the Eurasian continent. Significant warming to the west of Mongolia tends to weaken the north–south temperature gradient and the atmospheric baroclinicity to its south and eventually can lead to weakening of the midlatitude cyclone activity over East Asia.

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13

Liu, Jiawei, Haiming Xu, Jiechun Deng, Jing Ma und Leying Zhang. „Differences of East Asian Summer Monsoon Precipitation Responses between Transient and Stabilization Simulations“. Atmosphere 14, Nr. 12 (29.11.2023): 1763. http://dx.doi.org/10.3390/atmos14121763.

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The differences between the two global warming targets of the Paris Agreement, 1.5 °C and 2 °C above pre-industrial levels, have drawn much attention from the scientific community. However, there is a remaining gap to distinguish regional climate responses in these two most typical pathways, i.e., transient and stabilization simulations, toward specific warming levels. In this study, we discern the East Asia summer monsoon (EASM) responses between these two types of simulations at low-warming targets, based on the fully coupled community Earth system model (CESM). The two types of responses display a similar increase pattern in the EASM precipitation. However, the quantitative differences between these two types of responses are as large as those between the 1.5 °C and 2 °C warming scenarios. The moist budget analysis reveals that the EASM precipitation differences are mainly caused by the thermodynamic, dynamic, and transient eddy effects. Specifically, the thermodynamic effect contributes to the precipitation increment in the coastal area of East Asia in both types of responses, with the enhanced low-level specific humidity. The dynamic contribution shows tripolar and bipolar patterns in East Asia in the transient and stabilization responses, respectively. Remarkably, the transient eddy effect contribution emerges only in the stabilization responses. Further, we reveal the dominant role of the East Asian subtropical jet (EASJ) in determining the contributions from dynamic and transient eddy effects. The changes in the EASJ’s position and intensity are greatly regulated by the temperature change patterns at the mid-high levels in response to different greenhouse gas emission pathways. Our study highlights the differences between transient and stabilization climate states on a regional scale.

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14

Paloff, Benjamin. „East Is Always Further East“. East European Politics and Societies: and Cultures 28, Nr. 4 (November 2014): 687–92. http://dx.doi.org/10.1177/0888325414554697.

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15

Busheikin, Laura. „Gender Studies Inspirations East-East“. European Journal of Women's Studies 2, Nr. 1 (Februar 1995): 124–27. http://dx.doi.org/10.1177/135050689500200114.

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16

Wang, Zhili, Junyu Mu, Meilin Yang und Xiaochao Yu. „Reexamining the Mechanisms of East Asian Summer Monsoon Changes in Response to Non–East Asian Anthropogenic Aerosol Forcing“. Journal of Climate 33, Nr. 8 (15.04.2020): 2929–44. http://dx.doi.org/10.1175/jcli-d-19-0550.1.

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AbstractThis study examines the mechanisms by which the East Asian summer monsoon (EASM) changes in response to non–East Asian (NEA) anthropogenic aerosol forcing by distinguishing the fast direct atmospheric response and slow ocean-mediated response to forcing using a global aerosol–climate coupled model. The results show that NEA aerosol forcing significantly exacerbates the weakening of the EASM due to local aerosol forcing. The fast response is dominant in the weakening of the EASM and an anomalous precipitation pattern over eastern China resembling the “southern flood and northern drought” pattern in the total response to NEA aerosol forcing. Changes in upper-tropospheric temperature caused by the fast response play a major role in the impact of NEA aerosol forcing on the EASM. Anomalous cooling occurs during summer in the upper troposphere (at ~40°N) over East Asia caused by the fast response. This is due to the combined effects of strong eastward cold advection in the Northern Hemisphere midlatitudes caused by increased aerosol loading in Europe and the resulting change in local meridional heat transport in East Asia. Subsequently, the zonal wind speed changes on either side of the anomalous cooling, and the East Asian subtropical jet shifts equatorward, thereby weakening the EASM. The changes in atmospheric temperature and the local Hadley cell caused by the slow response to NEA aerosol forcing are conducive to strengthening the southwesterly winds over eastern China. Our study suggests the importance of NEA aerosol forcing in driving changes in the EASM on a fast time scale.

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17

Ahamed, Akkas. „Bangladesh-East Asia Relations in the Context of Bangladesh’s Look East Policy“. British Journal of Arts and Humanities 1, Nr. 4 (20.08.2019): 1–13. http://dx.doi.org/10.34104/bjah.019.0113.

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18

Hanser, Eva-Maria. „“How the East Sees the East”“. East Central Europe 43, Nr. 3 (03.12.2016): 278–97. http://dx.doi.org/10.1163/18763308-04303005.

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As the Slovenian art collective Neue Slowenische Kunst appropriates artefacts from different sources, the following paper attempts to clarify the significance of appropriation in relation to Russia. Three different artistic moments from different decades are chosen as starting points and key moments in order to examine nsk’s artistic approach.

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19

Suonsilta, R. „East or far east? [manufacturing outsourcing]“. Manufacturing Engineer 83, Nr. 4 (01.08.2004): 32–35. http://dx.doi.org/10.1049/me:20040406.

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20

Roy, Himanshu. „North-East and East-Asian Market“. Indian Journal of Public Administration 62, Nr. 3 (Juli 2016): 516–21. http://dx.doi.org/10.1177/0019556120160312.

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21

Lo, Adrienne. „East Is East, West Is West“. Journal of Linguistic Anthropology 15, Nr. 2 (Dezember 2005): 289–90. http://dx.doi.org/10.1525/jlin.2005.15.2.289.

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22

TREMBLAY, JEAN-FRANCOIS. „TO GO EAST OR FARTHER EAST“. Chemical & Engineering News 83, Nr. 12 (21.03.2005): 32–33. http://dx.doi.org/10.1021/cen-v083n012.p032.

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23

Delvoie, Louis A. „Review: Middle East: Middle East Dilemma“. International Journal: Canada's Journal of Global Policy Analysis 54, Nr. 4 (Dezember 1999): 729–31. http://dx.doi.org/10.1177/002070209905400432.

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24

Shebalina, E. O. „Is East Turning to the East?“ MGIMO Review of International Relations 17, Nr. 2 (22.04.2024): 160–67. http://dx.doi.org/10.24833/2071-8160-2024-2-95-160-167.

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25

Wang, Hongli, Xiaoning Xie und Xiaodong Liu. „On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results“. Advances in Meteorology 2015 (2015): 1–8. http://dx.doi.org/10.1155/2015/397395.

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Using outputs from 10 CMIP5 models with fixed sea surface temperature, we investigate the fast response of the East Asian summer monsoon (EASM) and summer precipitation in East China to anthropogenic aerosols. To address this topic, we employ two commonly used EASM indices that can represent zonal and meridional land-sea thermal contrast, respectively. The results reveal that the notion of a weakened EASM in response to increased anthropogenic aerosols is a robust one, as well as decreased precipitation in East China. The ensemble mean of decreased precipitation in the aerosol run was about 6.6% in comparison to the CTL run and could be enlarged to 8.3% by excluding the experiments with the aerosol direct effect only. Convective precipitation was found to be the primary contributor (>80%) to the reduction of total precipitation. The combination of direct and indirect effects of aerosols can decrease solar radiation reaching the Earth’s surface and eventually modulate large-scale EASM circulation and suppress summer precipitation in East China. The uncertainties and discrepancies among the models highlight the complexity of interaction in aerosol-precipitation processes when investigating present and future changes of the EASM.

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26

Yang, Yu, Dayong Wen, Shu Gui, Ruowen Yang und Jie Cao. „Thermal and Mechanical Effects of the Southeast Asian Low-Latitude Highlands on the East Asian Summer Monsoon“. Journal of Climate 37, Nr. 1 (01.01.2024): 349–61. http://dx.doi.org/10.1175/jcli-d-22-0814.1.

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Abstract The thermal and mechanical effects of the regional orography have long been recognized as the two most important factors driving the East Asian summer monsoon (EASM). The Southeast Asian low-latitude highlands (SEALLH) are a warmer and wetter highland region adjacent to the southeastern margin of the Tibetan Plateau. However, the importance of the individual contributions of the thermal and mechanical effects of the SEALLH to the EASM is still unclear. Results of numerical experiments show that the thermal effect of the SEALLH contribute to the precipitation and upper-tropospheric circulation of the EASM by roughly the same magnitude as the mechanical effect of the SEALLH, when its original height is reduced by 50%. The thermal effect of the SEALLH influences the EASM by exciting an East Asia–Pacific-like teleconnection, whereas the mechanical effect of the SEALLH impacts the EASM by exciting an equivalent barotropic Bay of Bengal–East Asia–Pacific-like teleconnection. This study could provide a new perspective for a better understanding of the EASM. Significance Statement Recent studies have shown that the mountains adjacent to the Tibetan Plateau have significant effects on the Asian summer monsoon, although these mountains are much lower in elevation and smaller in extent than the Tibetan Plateau. The Southeast Asian low-latitude highlands (SEALLH), located on the southeastern margin of the Tibetan Plateau, influence the East Asian summer monsoon (EASM) via both thermal and mechanical effects. However, the individual thermal and mechanical contributions to the EASM have not yet been clarified. Numerical experiments designed specifically for the SEALLH, which is warmer and wetter than the Tibetan Plateau, show that the thermal effect of the SEALLH on precipitation and the upper-tropospheric circulation over the EASM region is roughly equivalent to the mechanical effect of the SEALLH when its original height was reduced by 50%, but via different physical processes. The thermal effect of the SEALLH induces southerly wind anomalies between the SEALLH and the western North Pacific, influencing the EASM by exciting an East Asia–Pacific-like wave train. The mechanical effect of the SEALLH influences the EASM by exciting an equivalent barotropic Bay of Bengal–East Asia–Pacific-like wave train.

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Zhang, Pengfei, Yimin Liu und Bian He. „Impact of East Asian Summer Monsoon Heating on the Interannual Variation of the South Asian High“. Journal of Climate 29, Nr. 1 (22.12.2015): 159–73. http://dx.doi.org/10.1175/jcli-d-15-0118.1.

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Abstract Occupying the upper troposphere over subtropical Eurasia during boreal summer, the South Asian high (SAH) is thought to be a regulator of the East Asian summer monsoon (EASM), which is particularly important for regional climate over Asia. However, there is feedback of the condensational heating associated with EASM precipitation to SAH variability. In this study, interannual variation of SAH intensity and the mechanisms are investigated. For strong SAH cases, the high pressure system intensifies and expands. Significant positive anomalies of the geopotential height and upper-tropospheric temperature were found over the Middle East and to the east of the Tibetan Plateau (TP), namely, the western and the eastern flanks of the SAH. The dynamical diagnosis and the numerical experiments consistently show that the interannual variation of SAH intensity is strongly affected by EASM precipitation over the eastern TP–Yangtze River valley. The feedback of the condensational heating anomaly to the SAH is summarized as follows: Excessive EASM heating excites a local anticyclone in the upper troposphere and warms the upper troposphere, leading to the eastward extension of the SAH’s eastern edge and reinforcing geopotential height anomalies over East Asia. Furthermore, the monsoonal heating excites a westward-propagating Rossby wave that increases the upper-tropospheric geopotential height and warms the upper troposphere over the Middle East. In conclusion, this study suggests a mechanistic paradigm in which the EASM may also be a modulator of SAH variation rather than just a passive result of the latter as traditionally thought. The results suggest that the EASM and the SAH are a tightly interactive system.

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Huyan, Lidou, Jianping Li, Sen Zhao, Cheng Sun, Di Dong, Ting Liu und Yufei Zhao. „The Impact of Layer Perturbation Potential Energy on the East Asian Summer Monsoon“. Journal of Climate 30, Nr. 17 (September 2017): 7087–103. http://dx.doi.org/10.1175/jcli-d-16-0729.1.

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This paper analyzes the relationship between the 1000–850-hPa layer perturbation potential energy (LPPE) as the difference in local potential energy between the actual state and the reference state and the East Asian summer monsoon (EASM) using reanalysis and observational datasets. The EASM is closely related to the first-order moment term of LPPE (LPPE1) from the preceding March to the boreal summer over three key regions: the eastern Indian Ocean, the subtropical central Pacific, and midlatitude East Asia. The LPPE1 pattern (−, +, +), with negative values over the eastern Indian Ocean, positive values over the subtropical central Pacific, and positive values over East Asia, corresponds to negative LPPE1 anomalies over the south of the EASM region but positive LPPE1 anomalies over the north of the EASM region, which lead to an anomalous downward branch over the southern region but an upward branch over the northern region. The anomalous vertical motion affects the local meridional circulation over East Asia that leads to a southwesterly wind anomaly over East Asia (south of 30°N) at 850 hPa and anomalous downward motion over 100°–120°E (along 25°–35°N), resulting in a stronger EASM, more kinetic energy over the EASM region, and less boreal summer rainfall in the middle and lower reaches of the Yangtze River valley (24°–36°N, 90°–125°E). These LPPE1 anomalies in the eastern Indian Ocean and subtropical central Pacific appear to be connected to changes in local sea surface temperature through the release of latent heat.

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LEE, Jae-hwan. „East Palaces in Ancient East Asia and the East Palace of Silla“. Journal of Korean Ancient History 100 (31.12.2020): 115–44. http://dx.doi.org/10.37331/jkah.2020.12.100.115.

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30

Trimurti, Sus, Andi Sarina und Lariman . „Herpetofauna Distribution and Ecology in East Kutai District, East Kutai, East Kalimantan“. Volume 5 - 2020, Issue 8 - August 5, Nr. 8 (21.08.2020): 279–84. http://dx.doi.org/10.38124/ijisrt20aug192.

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Herpetofauna consisting of reptiles and amphibians is a group of fauna whose biodiversity potential is rarely known and is not well known by the public. The purpose of this study was to determine the distribution, ecology and diversity of herpetofauna in Mesangat Wetlands. The method used in this research is the Visual Encounter Survey (VES) search method by searching directly for the type of herpetofauna around the predetermined pathway. Field orientation is carried out to determine the location of the observation, the location of the observation is divided into 3 locations (Mesangat Hilir, Tengah and Hulu) in one observation location there are 5 stations (lanes) for herpetofauna observation. Observations were made in the morning starting at 09.00 - 12.00 WITA and at night starting at 20.00 - 23.00 WITA. Recorded data related to the number of individuals, activities, time found, environmental parameters and measured SVL if possible. Identified species were found using the identification key book Field Frogs of Borneo Inger and Stuebing (2014) and A Field Guide to the Snakes of Borneo Stuebing, Inger and Lardner (2014). The data were analyzed using Microsoft Excel 2010. The results showed that the distribution of herpetofauna in Mesangat Wetlands was fairly evenly distributed and the ecology of Mesangat Wetlands supported for herpetofauna life and the diversity index value obtained was 1.53 which was classified as medium category.

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Li, Li, und Yaocun Zhang. „Effects of Different Configurations of the East Asian Subtropical and Polar Front Jets on Precipitation during the Mei-Yu Season“. Journal of Climate 27, Nr. 17 (28.08.2014): 6660–72. http://dx.doi.org/10.1175/jcli-d-14-00021.1.

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Abstract Observational analysis indicates that the East Asian jet stream consists of two separate branches: the East Asian subtropical jet (EASJ) and the East Asian polar front jet (EAPJ). The impacts of different intensity configurations of the EASJ and EAPJ on precipitation during the mei-yu season are investigated using the NCEP–NCAR Reanalysis Project (NNRP) dataset and daily gauge observations in East China. The intensity and location of precipitation are associated with different configurations of the EASJ and EAPJ. Precipitation intensity increases with intensification of the EASJ and EAPJ. The rainband is located to the north of the mei-yu region when the EASJ intensifies and the EAPJ weakens. Further analyses indicate that the intensity changes of the EASJ and EAPJ are linked to the cold and warm airmass activities. For cases with strong EASJ and EAPJ, both the warm-moist and cold air masses are active. When the warm-moist and cold air masses meet near 30°N, abundant precipitation occurs in the Yangtze-Huai River basin (YHRB). For cases with weak EASJ and EAPJ, both the cold and warm-moist air masses are inactive, and no significant precipitation occurs in the YHRB. For cases with strong EASJ and weak EAPJ, the warm-moist air mass moves northward while the cold air mass is weak. Precipitation concentrates to the north of YHRB. For cases with weak EASJ and strong EAPJ, cold air extends farther south while the warm-moist air mass is inactive. Precipitation occurs to the south of YHRB.

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Lewis, George H., und James L. Watson. „Golden Arches East: McDonald's in East Asia“. Canadian Journal of Sociology / Cahiers canadiens de sociologie 24, Nr. 4 (1999): 571. http://dx.doi.org/10.2307/3341798.

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Lee, Hyun-Jung, Katsuhiko Yoshikawa und Carol Wasbauer Reade. „Intercultural Communication Challenges in East-East Encounters“. Academy of Management Proceedings 2018, Nr. 1 (August 2018): 10237. http://dx.doi.org/10.5465/ambpp.2018.6.

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Reese, R. Allan. „Graphical interpretations of data: East is east…“. Significance 16, Nr. 1 (Februar 2019): 42–44. http://dx.doi.org/10.1111/j.1740-9713.2019.01237.x.

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Casterline, John B., und David R. Phillips. „Ageing in East and South-East Asia.“ Population and Development Review 20, Nr. 2 (Juni 1994): 469. http://dx.doi.org/10.2307/2137531.

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Hermalin, Albert I. „Ageing in East and South-East Asia“. Population Studies 48, Nr. 3 (01.11.1994): 548–49. http://dx.doi.org/10.1080/0032472031000148156.

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Sandor, Paul. „East meets West in the Middle East“. Journal of Psychosomatic Research 61, Nr. 3 (September 2006): 283–84. http://dx.doi.org/10.1016/j.jpsychores.2006.08.002.

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38

Esterik, Penny Van, und James Watson. „Golden Arches East: McDonald's in East Asia“. Anthropologica 41, Nr. 1 (1999): 77. http://dx.doi.org/10.2307/25605923.

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39

Bajpaee, Chietigj. „Dephasing India's Look East/Act East Policy“. Contemporary Southeast Asia 39, Nr. 2 (31.08.2017): 348–72. http://dx.doi.org/10.1355/cs39-2d.

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Sharbaugh, Abigail. „Golden Arches East, McDonald's in East Asia“. Nutritional Anthropology 25, Nr. 2 (September 2002): 49–51. http://dx.doi.org/10.1525/nua.2002.25.2.49.

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41

Sarkar, Mitali. „Crisis in East and South East Asia“. Vikalpa: The Journal for Decision Makers 23, Nr. 4 (Oktober 1998): 51–60. http://dx.doi.org/10.1177/0256090919980406.

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This special volume of abstracts, focused on the East Asian economic crisis, captures the interpretations of various experts in the field. These extended abstracts are based on selected articles and speeches reflecting on the rise and fall of these economies, on the probable causes and the suggested cures, and on their implications for the different economies, including India. We look forward to your comments on this special volume. Abstracts of Indian Management Research is a regular feature of Vikalpa and is sponsored by the Indian Council of Social Science Research.

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Ren, Xuejuan, Xiuqun Yang und Cuijiao Chu. „Seasonal Variations of the Synoptic-Scale Transient Eddy Activity and Polar Front Jet over East Asia“. Journal of Climate 23, Nr. 12 (15.06.2010): 3222–33. http://dx.doi.org/10.1175/2009jcli3225.1.

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Abstract Seasonal variations of the synoptic-scale transient eddy activity (STEA) and the jet streams over East Asia are examined through analysis of the 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) data. Extracted from the 6-hourly upper-level wind fields, the distribution of the jet core numbers exhibits a distinct geographical border for the East Asian subtropical jet (EASJ) and the East Asian polar front jet (EAPJ) at the latitudes of the northern Tibetan Plateau (TP). In the cool seasons, two branches of the STEA and low-level baroclinicity exist over the East Asian landmass, accompanied by the two-jet state of the EASJ and EAPJ. In the warm seasons, a single jet pattern of the EASJ along the north flank of the TP is accompanied by the weakened STEA over the mid- to high latitudes of East Asia. Further analysis shows two distinct features of the seasonal variations of the STEA over East Asia, compared with that over the North Pacific. First, during the transitional period of April–June, the main STEA band over East Asia migrates northward dramatically, in conjunction with the EAPJ shifting in the same direction. Second, both the upper-level STEA and the lower-level baroclinicity poleward of the TP are prosperous in spring. The relationship between the STEA, baroclinicity, vertical wind shear, and static stability in the EAPJ region in different seasons is further investigated. It is found that in addition to the time-mean wind fields, the rapid increase in the sensible heat flux poleward side of the TP region in spring and the associated boundary layer processes are partially responsible for the spring prosperity of the local baroclinicity and the STEA.

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Wang, Yingsi, Tiangui Xiao, Xuefeng Dong, Yueqing Li, Wei Huang und Jie Tan. „Influence of 30–60 Days Intraseasonal Oscillation of East Asian Summer Monsoon on Precipitation in Southwest China“. Atmosphere 13, Nr. 8 (02.08.2022): 1222. http://dx.doi.org/10.3390/atmos13081222.

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The intraseasonal oscillation (ISO) of the East Asian summer monsoon (EASM) is an important factor affecting summer precipitation in China, but the relationship between the ISO of the EASM and summer precipitation in southwest China is currently still unclear. The relationship between the two is discussed, and the following conclusions are drawn: (1) there is a significant positive correlation between East Asian monsoon surge intensity and summer precipitation in southwest China. When the monsoon surge is stronger (weaker), the precipitation in southwest China is more (less). However, the areas where the monsoon surge has a more obvious effect on the summer precipitation in southwest China are mainly located east of 105° E, and the monsoon surge has no obvious effect on the area west of 105° E. This may be more (less) the case in monsoon surge years, when a low-frequency oscillation of 30–60 days (10–20 days) plays a dominant role. The East Asian region has a longitudinal wave train of “+ − +” (“− + −“), the western Pacific subtropical high is westerly (easterly), the South China Sea and western Pacific is affected by anticyclone (cyclone), the EASM is active (suppressive), eastern southwest China has water vapor convergence (divergence) and upward (downward) airflow. (2) We found that 1998 was a typical year for the 30–60 days ISO of the EASM. There are two obvious 30–60 days oscillation cycles. In this year, when the intensity of the ISO of the EASM increases (decreases), the range of positive precipitation anomaly region in southwest China extends (decreases). The atmospheric circulation characteristics show that, when the western Pacific subtropical high is west (east) and south (north), and there is obvious anticyclonic (cyclonic) circulation in China–western Pacific, and the EASM is stronger (weaker), which leads to more (less) precipitation in southwest China.

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Chang, Kyung-Il, Chang-Keun Kang und Dong-Jin Kang. „East Asian Seas Time-series I (EAST-I)“. Ocean and Polar Research 32, Nr. 3 (30.09.2010): 267–68. http://dx.doi.org/10.4217/opr.2010.32.3.267.

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Li, Juan, Bin Wang und Young-Min Yang. „Diagnostic Metrics for Evaluating Model Simulations of the East Asian Monsoon“. Journal of Climate 33, Nr. 5 (01.03.2020): 1777–801. http://dx.doi.org/10.1175/jcli-d-18-0808.1.

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AbstractThe distinctive monsoon climate over East Asia, which is affected by the vast Eurasian continent and Pacific Ocean basin and the high-altitude Tibetan Plateau, provides arguably the best testbed for evaluating the competence of Earth system climate models. Here, a set of diagnostic metrics, consisting of 14 items and 7 variables, is specifically developed. This physically intuitive set of metrics focuses on the essential features of the East Asian summer monsoon (EASM) and East Asian winter monsoon (EAWM), and includes fields that depict the climatology, the major modes of variability, and unique characteristics of the EASM. The metrics are applied to multimodel historical simulations derived from 20 models that participated in phases 3 and 5 of the Coupled Model Intercomparison Project (CMIP3 and CMIP5, respectively), along with the newly developed Nanjing University of Information Science and Technology Earth System Model, version 3. The CMIP5 models show significant improvements over the CMIP3 models in terms of the simulated East Asian monsoon circulation systems on a regional scale, major modes of EAWM variability, the monsoon domain and precipitation intensity, and teleconnection associated with the heat source over the Philippine Sea. Clear deficiencies persist from CMIP3 to CMIP5 with respect to capturing the major modes of EASM variability, as well as the relationship between the EASM and ENSO during El Niño developing and decay phases. The possible origins that affect models’ performance are also discussed. The metrics provide a tool for evaluating the performance of Earth system climate models, and facilitating the assessment of past and projected future changes of the East Asian monsoon.

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Han, Han, Jane Liu, Huiling Yuan, Tijian Wang, Bingliang Zhuang und Xun Zhang. „Foreign influences on tropospheric ozone over East Asia through global atmospheric transport“. Atmospheric Chemistry and Physics 19, Nr. 19 (08.10.2019): 12495–514. http://dx.doi.org/10.5194/acp-19-12495-2019.

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Abstract. Tropospheric ozone in East Asia is influenced by the transport of ozone from foreign regions around the world. However, the magnitudes and variations in such influences remain unclear. This study was performed to investigate the influences using a global chemical transport model, GEOS-Chem, through the tagged ozone and emission perturbation simulations. The results show that foreign ozone is transported to East Asia (20–60∘ N, 95–150∘ E) mainly through the middle and upper troposphere. In East Asia, the influence of foreign ozone increases rapidly with altitude. In the middle and upper troposphere, the regional mean concentrations of foreign ozone range from 32 to 65 ppbv, being 0.8–4.8 times higher than its native counterpart (11–18 ppbv). Annually, ∼60 % of foreign ozone in the East Asian middle and upper troposphere comes from North America (5–13 ppbv) and Europe (5–7 ppbv), as well as from foreign oceanic regions (9–21 ppbv). Over the East Asian tropospheric columns, foreign ozone appears most in spring when ozone concentrations in the foreign regions are high and the westerlies are strong and least in summer when the South Asian High blocks eastward foreign ozone from reaching East Asia south of 35∘ N. At the East Asian surface, the annual mean of foreign ozone concentrations is ∼22.2 ppbv, which is comparable to its native counterpart of ∼20.4 ppbv. In the meantime, the annual mean of anthropogenic ozone concentrations from foreign regions is ∼4.7 ppbv, half of which comes from North America (1.3 ppbv) and Europe (1.0 ppbv). Seasonally, foreign ozone concentrations at the East Asian surface are highest in winter (27.1 ppbv) and lowest in summer (16.5 ppbv). This strong seasonality is largely modulated by the East Asian monsoon (EAM) via its influence on vertical motion. The large-scale subsidence prevailing during the East Asian winter monsoon (EAWM) favours the downdraft of foreign ozone to the surface, while widespread convection in the East Asian summer monsoon (EASM) blocks such transport. Interannually, the variation in foreign ozone at the East Asian surface is found to be closely related to the intensity of the EAM. Specifically, the stronger the EAWM is in a winter, the more ozone from North America and Europe reaches the East Asian surface because of the stronger subsidence behind the East Asian trough. In summer, ozone from South and South-east Asia is reduced in strong EASM years due to weakened south-westerly monsoon winds. This study suggests substantial foreign influences on ozone at the East Asian surface and in its tropospheric columns. It also underscores the importance of the EAM in the seasonal and interannual variations in foreign influences on surface ozone in East Asia.

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Bagus Hermawan, Aldi, Muhammad Yustitio Hadi Utomo, Pramudya Abimanyu, Visnhu Arya Bhisma, Nala Widyadhana, Rido Izril Qotana, Sujatmiko Dwi Kuncoro und Endang Sholihatin. „ANALYSIS OF INDONESIAN LANGUAGE PREFERENCES IN UPN "VETERAN" JAWA TIMUR STUDENTS AS WEBSITE-BASED INFORMATION SYSTEM USERS“. Matapena: Jurnal Keilmuan Bahasa, Sastra, dan Pengajarannya 6, Nr. 1 (17.06.2023): 75–86. http://dx.doi.org/10.36815/matapena.v6i01.2639.

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This study aims to determine the preferences of Indonesian among UPN "Veteran" East Java students as users of a website-based information system, to determine the factors that influence the preferences of Indonesian students at UPN "Veteran" East Java as users of a website-based information system, and to find out the differences in Indonesian language preference for East Java "Veteran" UPN students as users of a website-based information system. This study used a quantitative research method by distributing questionnaires for data collection. The results of this study show that the preference for Indonesian among UPN "Veteran" East Java students is still high, at around 95% in the use of a website-based information system. Factors that influence preference for Indonesian among UPN "Veteran" East Java students as users of a website-based information system are 1) the ease of understanding information, 2) the convenience factor, and 3) the quality of Indonesian translation. In addition, differences in Indonesian language preferences among UPN "Veteran" East Java students as users of website-based information systems are due to several factors, namely the level of comfort and familiarity with using Indonesian in using website-based information systems, the frequency of using Indonesian in everyday life, and the level of confidence in the quality of access and ease of use of website-based information systems in Indonesian.

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Diana Rapitasari. „Strategi Pemulihan Ekonomi Nasional di Jawa Timur melalui JATIM BANGKIT“. Majalah Ekonomi 26, Nr. 1 (19.07.2021): 62–70. http://dx.doi.org/10.36456/majeko.vol26.no1.a3954.

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The National Economic Recovery Strategy in East Java is really a plan or map to help leaders or direct organization in East Java in economic recovery efforts, handling the pandemic of Corona Virus Disease (COVID-19) or responding to threats that threaten the economy or financial system as well as economic rescue in East Java. This article was written using a qualitative descriptive method with interview and documentation techniques. The information of this research is officials who are in the Regional Development Planning Agency of East Java Province who are members of the National Economic Recovery Program in East Java through East Java Bangkit, so that the authors can present data systematically, factually and accurately regarding facts in the field. National Economic Recovery Strategies in East Java include recovery of trade and industrial activities, overcoming trade barriers both import duties and import export regulations, budget allocated for health and education in order to ease the burden on society, increase disposable income through creative efforts, encourage household consumption, which is a contributor to aggregate expenditure, continues the subsidy program for small industries and cooperatives as well as optimism for East Java's economic growth.

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Zhang, Wanxin, Haishan Chen, Liming Zhou, Botao Zhou, Jie Zhang und Jiangfeng Wei. „Effects of Nonuniform Land Surface Warming on Summer Anomalous Extratropical Cyclone Activity and the East Asian Summer Monsoon: Numerical Experiments with a Regional Climate Model“. Journal of Climate 33, Nr. 24 (15.12.2020): 10469–88. http://dx.doi.org/10.1175/jcli-d-20-0088.1.

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AbstractPrevious studies detected significant negative correlations between the nonuniform land surface warming and the decadal weakened activities of the summer extratropical cyclones (ECs) over East Asia and the East Asian summer monsoon (EASM) after the early 1990s. Here such relationships are further examined and the possible mechanisms are explored via numerical sensitivity experiments with a regional climate model (RegCM4.5). The positive/negative sensible heat flux (SH) anomalies were added as a forcing to a key region near 50°N of East Asia in RegCM4.5 to simulate the observed ground surface temperature (GST) anomalies. The model results suggest that the nonuniform land surface warming over the Lake Baikal area (50°–60°N, 90°–120°E) can indeed cause the weakening of the extratropical cyclogenesis and affect the decadal weakening of the EASM. Warm (cold) GST forcing over the key GST region can lead to decreasing (increasing) atmospheric baroclinicity and related energy conversion of the EC activity over the key EC region (40°–50°N, 90°–120°E), resulting in an evidently weakening (enhancing) of the ECs over East Asia. Meanwhile, precipitation shows a dipole pattern with significantly suppressed (enhanced) precipitation in northern and northeastern China, and slightly enhanced (suppressed) rainfall south of 40°N of East Asia, mainly over the East China Sea. Lake Baikal and its adjacent areas are occupied by a strong anticyclonic (cyclonic) circulation while the southeast coastal areas of China have a relatively weak cyclonic (anticyclonic) circulation accompanied with an anomalous northeasterly (southwesterly) wind to the southeast of the anticyclonic circulation, which is opposite to (coincident with) the atmospheric circulation anomalies that are associated with the second mode of the EASM.

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Zhao, Guijie, Gang Huang, Renguang Wu, Weichen Tao, Hainan Gong, Xia Qu und Kaiming Hu. „A New Upper-Level Circulation Index for the East Asian Summer Monsoon Variability“. Journal of Climate 28, Nr. 24 (15.12.2015): 9977–96. http://dx.doi.org/10.1175/jcli-d-15-0272.1.

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Abstract The East Asian summer monsoon (EASM) and its variability involve circulation systems in both the tropics and midlatitudes as well as in both the lower and upper troposphere. Considering this fact, a new EASM index (NEWI) is proposed based on 200-hPa zonal wind, which takes into account wind anomalies in the southern (about 5°N), middle (about 20°N), and northern areas (about 35°N) of East Asia. The NEWI can capture the interannual EASM-related climate anomalies and the interdecadal variability well. Compared to previous indices, the NEWI shows a better performance in describing precipitation and air temperature variations over East Asia. It can also show distinct climate anomalous features in early and late summer. The NEWI is tightly associated with the East Asian–Pacific or the Pacific–Japan teleconnection, suggesting a possible role of internal dynamics in the EASM variability. Meanwhile, the NEWI is significantly linked to El Niño–Southern Oscillation and tropical Indian Ocean sea surface temperature anomalies. Furthermore, the NEWI is highly predictable in the ENSEMBLES models, indicating its advantage for operational prediction of the EASM. The physical mechanism of the EASM variability as represented by the NEWI is also explicit. Both warm advection anomalies of temperature by anomalous westerly winds and the advection of anomalous positive relative vorticity by northerly basic winds cause anomalous ascending motion over the mei-yu–changma–baiu rainfall area, and vice versa over the South China Sea area. Hence, this NEWI would be a good choice to study, monitor, and predict the EASM.

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