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Journal articles on the topic 'Subtropical Asia'

Author: Grafiati

Published: 7 June 2025

Last updated: 2 August 2025

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1

Zhu, Hua, and Yunhong Tan. "The Origin of Evergreen Broad-Leaved Forests in East Asia from the Evidence of Floristic Elements." Plants 13, no. 8 (2024): 1106. http://dx.doi.org/10.3390/plants13081106.

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Arguments about the origin and evolution of the evergreen broad-leaved forests in East Asia exist generally, and are even contradictory in some cases. The origin and evolution of the flora of East Asia, especially in the evolutionary process, the formation time of the Asian monsoon, the implications of phylogenetic and biogeographic studies on some important taxa, and the implications of palaeobotanical evidence are debatable. Most research from different disciplines suggests that the monsoon in the Miocene was key to the diversification of East Asian flora and its evergreen broad-leaved fores

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2

Shi, Tao, Tian Weiteng, Wei Zhang, and Qian Zhou. "Spatiotemporal Relationship Between Ecological Environment and Economic Development in Tropical and Subtropical Regions of Asia." Tropical Conservation Science 12 (January 2019): 194008291987896. http://dx.doi.org/10.1177/1940082919878961.

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This article is devoted to study the coordination coupling relationship between economic development and ecological environment in tropical and subtropical regions of Asia to reflect the spatiotemporal heterogeneity of the coordination in different regions. Using the entropy method and Geographically and Temporally Weighted Regression model, we empirically analyze 14 tropical and subtropical countries in Asia from 2003 to 2016. The empirical results show that most of the tropical and subtropical sample countries in Asia are at an intermediate coordination coupling level between economic develo

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3

Zhu, Zhiwei, and Tim Li. "A New Paradigm for Continental U.S. Summer Rainfall Variability: Asia–North America Teleconnection." Journal of Climate 29, no. 20 (2016): 7313–27. http://dx.doi.org/10.1175/jcli-d-16-0137.1.

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Abstract The present study reveals a close relationship between the leading mode of continental U.S. (CONUS) summer rainfall and the East Asian subtropical monsoon rainfall (viz., mei-yu in China, baiu in Japan, and changma in the Korean peninsula). The East Asian subtropical monsoon rainfall and the CONUS dipole rainfall patterns are connected by an upper-level Asia–North America (ANA) teleconnection. The Rossby wave energy propagates along the path of the westerly jet stream (WJS) from East Asia to North America, affecting the CONUS summer rainfall. Mechanisms through which East Asian summer

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4

Lu, Riyu, and Zhongda Lin. "Role of Subtropical Precipitation Anomalies in Maintaining the Summertime Meridional Teleconnection over the Western North Pacific and East Asia." Journal of Climate 22, no. 8 (2009): 2058–72. http://dx.doi.org/10.1175/2008jcli2444.1.

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Abstract The meridional teleconnection patterns over the western North Pacific and East Asia (WNP–EA) during summer have a predominant role in affecting East Asian climate on the interannual time scale. A well-known seesaw pattern of tropical–subtropical precipitation is associated with the meridional teleconnection, and the subtropical precipitation anomaly has been previously viewed as a result of anomalous circulations associated with the teleconnection. In this study, however, the authors suggest that subtropical precipitation anomalies, in turn, can significantly affect large-scale circul

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Park, Hyo-Seok, Benjamin R. Lintner, William R. Boos, and Kyong-Hwan Seo. "The Effect of Midlatitude Transient Eddies on Monsoonal Southerlies over Eastern China." Journal of Climate 28, no. 21 (2015): 8450–65. http://dx.doi.org/10.1175/jcli-d-15-0133.1.

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Abstract The strengthening of monsoonal southerlies over East Asia is associated with the westward intensification of the North Pacific subtropical high. Previous work has shown that the seasonal-mean position and strength of subtropical highs are affected by tropical and subtropical diabatic heating. Here it is shown that the synoptic-time-scale strengthening of southerlies over eastern China is dynamically tied to extratropical eddy activity. Composite analysis based on strong southerly wind events highlights an antecedent baroclinic wave train propagating southeastward into eastern China fr

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6

Yang, Song, K.-M. Lau, S.-H. Yoo, J. L. Kinter, K. Miyakoda, and C.-H. Ho. "Upstream Subtropical Signals Preceding the Asian Summer Monsoon Circulation." Journal of Climate 17, no. 21 (2004): 4213–29. http://dx.doi.org/10.1175/jcli3192.1.

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Abstract In this study, the authors address several issues with respect to the antecedent signals of the large-scale Asian summer monsoon that were earlier identified by Webster and Yang. In particular, they revisit the changes in the subtropical upper-tropospheric westerlies preceding the monsoon, depict the detailed structure of the monsoon's antecedent signals, and investigate the physical processes from the signals to the monsoon. They also explore the teleconnection of these signals to various large-scale climate phenomena and emphasize the importance of the upstream location of the signa

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7

Siu, Leong Wai, and Kenneth P. Bowman. "Forcing of the Upper-Tropospheric Monsoon Anticyclones." Journal of the Atmospheric Sciences 76, no. 7 (2019): 1937–54. http://dx.doi.org/10.1175/jas-d-18-0340.1.

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Abstract During the boreal warm season (May–September), the circulation in the upper troposphere and lower stratosphere is dominated by two large anticyclones: the Asian monsoon anticyclone (AMA) and North American monsoon anticyclone (NAMA). The existence of the AMA has long been linked to Asian monsoon precipitation using the Matsuno–Gill framework, but the origin of the NAMA has not been clearly understood. Here the forcing mechanisms of the NAMA are investigated using a simplified dry general circulation model. The simulated anticyclones are in good agreement with observations when the mod

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8

Garfin-Woll, Gregg M. "Interannual Variability of Asian Monsoon Precipitation, 1953-1982, Using Instrumental Records." IAWA Journal 20, no. 3 (1999): 227–38. http://dx.doi.org/10.1163/22941932-90000686.

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Instrumental records were used to assess the interannual variability of precipitation for the greater Asian monsoon region (50°N-15°S, 60°E-150°E). Correlation analysis shows intriguing teleconnections between subtropical and midlatitude precipitation regions. Principal components analyses show that ENSO (EI Niño-Southern Oscillation) is the dominant factor associated with recent interannual variation of precipitation in the region. The strongest relationships between ENSO and boreal summer precipitation were found in subtropical regions, as weIl as North Central China and southeastern Kazakhs

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9

Chen, Junming, Ping Zhao, Song Yang, Ge Liu, and Xiuji Zhou. "Simulation and Dynamical Prediction of the Summer Asian–Pacific Oscillation and Associated Climate Anomalies by the NCEP CFSv2." Journal of Climate 26, no. 11 (2013): 3644–56. http://dx.doi.org/10.1175/jcli-d-12-00368.1.

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Abstract The Asian–Pacific Oscillation (APO) is a dominant teleconnection pattern linking the climate anomalies over Asia, the North Pacific, and other regions including North America. The National Centers for Environmental Prediction (NCEP) Climate Forecast System version 2 (CFSv2) successfully simulates many summer-mean features of the upper-tropospheric temperature, the South Asian high, the westerly and easterly jet streams, and the regional monsoons over Asia and Africa. It also well simulates the interannual variability of the APO and associated anomalies in atmospheric circulation, prec

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10

Kim, Min-Seok, Peng Zhang, Sung-Ho Woo, Youngdae Koh, Hans W. Linderholm, and Jee-Hoon Jeong. "The Potential of Using Tree-Ring Chronology from the Southern Coast of Korea to Reconstruct the Climate of Subtropical Western North Pacific: A Pilot Study." Atmosphere 11, no. 10 (2020): 1082. http://dx.doi.org/10.3390/atmos11101082.

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Tree-ring width (TRW) chronologies have successfully been used as climate proxies to infer climate variabilities over the past hundreds to thousands of years worldwide beyond observational records. However, these data are scarce over parts of subtropical East Asia, and especially over the Korean Peninsula. In this pilot study, Korean red pine (Pinus densiflora Siebold and Zucc.) TRW chronologies from Mt. Mudeung and Mt. Wolchul, South Korea, were developed, and their local- to large-scale climatic responses were investigated. Mt. Mudeung TRW had a positive association with local temperature in

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11

Mitra, S. K., P. K. Pathak, and I. Chakraborty. "UNDERUTILIZED TROPICAL AND SUBTROPICAL FRUITS OF ASIA." Acta Horticulturae, no. 770 (June 2008): 67–76. http://dx.doi.org/10.17660/actahortic.2008.770.7.

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12

Xu, Peiqiang, Lin Wang, and Jie Ming. "Central Asian Precipitation Extremes Affected by an Intraseasonal Planetary Wave Pattern." Journal of Climate 35, no. 8 (2022): 2603–16. http://dx.doi.org/10.1175/jcli-d-21-0657.1.

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Abstract The characteristics and mechanisms of extreme precipitation events over central Asia are investigated based on daily data and percentile criteria. The composited extreme precipitation events have a life cycle of about 10 days. The precipitation signal is weak but significant from eight to two days before the peak. Then it amplifies rapidly and reaches its peak in two days. The earliest precipitation signal appears over the northwest of central Asia and moves southeastward. It maximizes over northern central Asia and the windward side of the mountainous region, suggesting the role of o

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13

Wu, Chi-Hua. "Seasonal adjustment of particulate matter pollution in coastal East Asia during the 2020 COVID lockdown." Environmental Research Letters 16, no. 12 (2021): 124023. http://dx.doi.org/10.1088/1748-9326/ac343c.

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Abstract Seasonally, the East Asian particulate matter (PM) level is higher in the winter–spring period than in summer, at which time the level rapidly decreases due to the summer monsoon migration. Attempting to attribute East Asian PM pollution to a source without considering such natural factors is challenging. However, to what degree the effect of season on an attribution bias remains controversial; the bias may even be implicated in PM-related health effects. This study examined seasonal dynamics including the unusual precipitation evolution during 2020—a year in which coronavirus-related

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14

Huyan, Lidou, Jianping Li, Sen Zhao, et al. "The Impact of Layer Perturbation Potential Energy on the East Asian Summer Monsoon." Journal of Climate 30, no. 17 (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, posi

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15

Han, Han, Jane Liu, Huiling Yuan, et al. "Characteristics of intercontinental transport of tropospheric ozone from Africa to Asia." Atmospheric Chemistry and Physics 18, no. 6 (2018): 4251–76. http://dx.doi.org/10.5194/acp-18-4251-2018.

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Abstract. In this study, we characterize the transport of ozone from Africa to Asia through the analysis of the simulations of a global chemical transport model, GEOS-Chem, from 1987 to 2006. The receptor region Asia is defined within 5–60∘ N and 60–145∘ E, while the source region Africa is within 35∘ S–15∘ N and 20∘ W–55∘ E and within 15–35∘ N and 20∘ W–30∘ E. The ozone generated in the African troposphere from both natural and anthropogenic sources is tracked through tagged ozone simulation. Combining this with analysis of trajectory simulations using the Hybrid Single-Particle Lagrangian In

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16

Zhou, Houyun, Jianxin Zhao, Pingzhong Zhang, et al. "Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d." Quaternary Research 70, no. 2 (2008): 315–21. http://dx.doi.org/10.1016/j.yqres.2008.04.007.

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AbstractThe Asian monsoon is an important component of the global climate system. Seasonal variations in wind, rainfall, and temperature associated with the Asian monsoon systems affect a vast expanse of tropical and subtropical Asia. Speleothem-derived summer monsoon variation in East Asia was previously found to be closely associated with millennial-scale change in temperature in the North Atlantic region between 75 and 10 ka. New evidence recovered from East Asia, however, suggests that the teleconnection between summer monsoon in East Asia and temperature change in the North Atlantic regio

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17

Tanno, Nonaki, Masayoshi Nakayama, Hirofumi Yashima, et al. "Gibberellins A19 and A24 from Yams, Dioscorea bulbifera, D. pentaphylla and D. oppositifolia." Zeitschrift für Naturforschung C 49, no. 7-8 (1994): 399–403. http://dx.doi.org/10.1515/znc-1994-7-801.

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Gibberellin A19 (GA19) and GA24 were identified by gas chromatography-mass spectrometry from growing shoots of four strains of three species of D ioscorea, D. bulbifera var. vera, D. pentaphylla and D. oppositifolia (yams), which are distributed in the subtropical and tropical regions of Asia. An earlier report indicated the presence of several GAs including GA19 and GA24 in a cultivated temperate species of East Asia, D. opposita; these findings suggest possible coexistence of two GA biosynthetic pathways, early 13-hydroxylation and non-13-hydroxylation pathways comm only in Asian species of

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18

Watanabe, Takeshi, and Koji Yamazaki. "Influence of the Anticyclonic Anomaly in the Subtropical Jet over the Western Tibetan Plateau on the Intraseasonal Variability of the Summer Asian Monsoon in Early Summer." Journal of Climate 25, no. 4 (2012): 1291–303. http://dx.doi.org/10.1175/jcli-d-11-00036.1.

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Abstract The upper-level troposphere over the western Tibetan Plateau, where the subtropical jet is located in summer, is a region of marked intraseasonal variability in geopotential height (GPH). This study investigates the influence of an anomaly in this region on the summer Asian monsoon. To this end, the GPH index is defined as the daily geopotential height anomaly at 200 hPa over the region based on 40-yr European Centre for Medium-Range Weather Forecasts Re-Analysis (ERA-40) data. Composites with respect to strongly positive values of the GPH index are analyzed. The results indicate that

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19

Matsumura, Shinji, Takeshi Horinouchi, Shiori Sugimoto, and Tomonori Sato. "Response of the Baiu Rainband to Northwest Pacific SST Anomalies and Its Impact on Atmospheric Circulation." Journal of Climate 29, no. 8 (2016): 3075–93. http://dx.doi.org/10.1175/jcli-d-15-0691.1.

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Abstract The Pacific–Japan (PJ) teleconnection pattern leads to a meridional precipitation dipole between the subtropics and East Asia in the summer of El Niño decaying years. However, observational analysis and model experiments indicate that increased sea surface temperature (SST) in the Kuroshio–Oyashio Extension (KOE) region, where a strong northward-decreasing SST gradient occurs, induces a northward shift of baiu rainfall with the subtropical jet, forming a tripolar precipitation anomaly pattern over the northwest Pacific. In July, the leading empirical orthogonal function (EOF) mode for

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20

Li, Haishan, Ke Fan, Zhiqing Xu, and Hua Li. "Modified Three-Dimensional Jet Indices and Their Application to East Asia." Atmosphere 10, no. 12 (2019): 776. http://dx.doi.org/10.3390/atmos10120776.

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A set of three-dimensional jet indices (jet speed index, jet pressure index, jet latitude index) has been proposed in previous literature to describe the variation of jet streams in both the horizontal and vertical direction. We refer to these indices at the ‘AC’ indices, after the names of the researchers involved. However, the physical meaning of the AC indices and the relationship between AC indices and climate systems are not fully understood. Further study is still needed for applying the indices in East Asia (70°–140° E). In this study, based on the understanding of the physical meaning

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21

Abbas, Sohail, Mian Sabir Hussain, Safdar Ali Sherazi, Mareena Khurshid, and Saadia Sultan Wahla. "Connection between the South and East Asian Monsoons: Comparing Summer Monsoon Rainfall of Pakistan and South Korea." International Journal of Economic and Environmental Geology 11, no. 2 (2020): 6–11. http://dx.doi.org/10.46660/ijeeg.vol11.iss2.2020.438.

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This study investigates the tele-connection of the southeast Asian monsoon systems by comparing the summer monsoon (June to September) rainfall variability between Pakistan and south Korea. The daily data sets (19812014) of rainfall of Pakistan and south Korea are utilized to explore the possible link. The data products of the National Centers for Environmental Prediction and National Center for Atmospheric Research (NCEP/NCAR) were also used for the understanding of the large-scale atmospheric environments. The patterns of summer monsoon rainfall on a daily basis between Pakistan and south Ko

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WEN, J. "EVOLUTION OF THE ARALIA–PANAX COMPLEX (ARALIACEAE) AS INFERRED FROM NUCLEAR RIBOSOMAL ITS SEQUENCES." Edinburgh Journal of Botany 58, no. 2 (2001): 243–57. http://dx.doi.org/10.1017/s0960428601000610.

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The Aralia–Panax complex consists of three closely related genera of Araliaceae (Aralia L., Panax L. and Sciadodendron Griseb.), widely distributed in temperate, subtropical, and tropical regions of Asia and the Americas. Three major lineages (Panax, Aralia sect. Aralia, and Aralia sect. Dimorphanthus Miq.) are disjunctly distributed in eastern Asia and North America. Comparative sequencing of the internal transcribed spacer (ITS) regions of nuclear ribosomal DNA was carried out in order to examine the phylogenetic and biogeographic relationships of this complex. Results suggest Aralia is para

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23

WANG, FA-GUO, AI-HUA WANG, RONG-RONG HE, et al. "Phytogeography of pteridophytes on limestone areas in Guangdong, China." Phytotaxa 317, no. 2 (2017): 81. http://dx.doi.org/10.11646/phytotaxa.317.2.1.

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Guangdong Province, located in southern China, is of great interest in studies of plant geography and conservation in limestone areas because of its rich biodiversity. We: (1) performed a phytogeographical analysis of pteridophytes in the limestone areas in Guangdong, (2) evaluated and determined levels of endemism, and (3) identified affinities with the floras of neighboring limestone areas. We found that some families show a preference for limestone habitats, e.g., Hypodematiaceae, Lygodiaceae, and Adiantaceae, are typical elements among pteridophytes in the limestone regions of Guangdong. I

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Krüger, K., U. Langematz, J. L. Grenfell, and K. Labitzke. "Climatological features of stratospheric streamers in the FUB-CMAM with increased horizontal resolution." Atmospheric Chemistry and Physics 5, no. 2 (2005): 547–62. http://dx.doi.org/10.5194/acp-5-547-2005.

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Abstract. The purpose of this study is to investigate horizontal transport processes in the winter stratosphere using data with a resolution relevant for chemistry and climate modeling. For this reason the Freie Universität Berlin Climate Middle Atmosphere Model (FUB-CMAM) with its model top at 83 km altitude, increased horizontal resolution T42 and the semi-Lagrangian transport scheme for advecting passive tracers is used. A new approach of this paper is the classification of specific transport phenomena within the stratosphere into tropical-subtropical streamers (e.g. Offermann et al., 1999)

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Kelly, Patrick, and Brian Mapes. "Asian Monsoon Forcing of Subtropical Easterlies in the Community Atmosphere Model: Summer Climate Implications for the Western Atlantic." Journal of Climate 26, no. 9 (2013): 2741–55. http://dx.doi.org/10.1175/jcli-d-12-00339.1.

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Abstract The effects of a progressively enhanced Asian summer monsoon on the mean zonal wind are examined in a series of experiments using the Community Atmosphere Model version 4 (CAM4). The response of the barotropic mean zonal wind varies in a linear fashion with the forcings of 5, 10, and 20 W m−2 in net radiation over South Asia. The authors increase the strength of the monsoon by making the South Asian land surface hotter (via lower soil albedo). This leads to an enhanced Rossby wave source region over the Balkan Peninsula at 45°N, northwest of the upper-level Tibetan high (TH). Equatorw

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Shuckburgh, Emily, Francesco d’Ovidio, and Bernard Legras. "Local Mixing Events in the Upper Troposphere and Lower Stratosphere. Part II: Seasonal and Interannual Variability." Journal of the Atmospheric Sciences 66, no. 12 (2009): 3695–706. http://dx.doi.org/10.1175/2009jas2983.1.

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Abstract The Lyapunov diffusivity is used to investigate local isentropic mixing events in the upper troposphere–lower stratosphere (UTLS) region. The diagnostic highlights the seasonal cycle of the longitudinally varying mixing properties, in particular those associated with the monsoon circulations and the westerly ducts in the subtropics. The results are broadly consistent with studies of Rossby wave–breaking frequencies. The mixing structure is shown to be modulated by modes of atmospheric variability. El Niño–Southern Oscillation (ENSO) is found to strongly influence the mixing structure

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Li, Yang, Weitao Jin, Liguo Zhang, et al. "Biogeography and Diversification of the Tropical and Subtropical Asian Genus Gastrochilus (Orchidaceae, Aeridinae)." Diversity 14, no. 5 (2022): 396. http://dx.doi.org/10.3390/d14050396.

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Tropical and subtropical Asia are major orchid diversity and endemism centers. However, the evolutionary dynamics of orchids in these areas remain poorly studied. Gastrochilus D. Don, a species-rich orchid genus from tropical and subtropical Asian forests, was employed to investigate the issue. We firstly used eight DNA regions to reconstruct the phylogeny and estimate the divergence times within Gastrochilus. We inferred the ancestral ranges and conducted a diversification analysis based on empirical and simulated data. Subsequently, we assessed the ancestral niche state and tested for phylog

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Vaid, Bakshi Hardeep. "Changing Convection in Central Asia during the Seasonal Transitional Period and Region to Its West before and after 1999: Role of Upper Vertical Thermal Contrast." Atmosphere 14, no. 1 (2022): 59. http://dx.doi.org/10.3390/atmos14010059.

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The objective of this study is to investigate and understand the changes in thermal contrast in the upper troposphere over Central Asia before and after 1999. It was observed that there was a discernible increase/decrease in upper tropospheric temperature (TT) in the 100 hPa/250 hPa over the Central Asian region during PRE99, whereas during POST99, it was found to be the other way around. A clear increase and decrease in the upper TT pattern in 100 hPa and 250 hPa can be attributed to anti-cyclonic and cyclonic circulations in the wind shear, respectively. The subtropical jet has been shown to

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Khurramov, Sh Kh, and A. S. Bekmuradov. "Parasitic nematodes of wild and cultivated subtropical fruit plants in Central Asia." Russian Journal of Parasitology 15, no. 1 (2021): 98–102. http://dx.doi.org/10.31016/1998-8435-2021-15-1-98-102.

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The purpose of the research is studying the species composition and control measures against parasitic nematodes of wild and cultivated subtropical fruit plants of Central Asia.Materials and methods. We studied subtropical fruit crops in 198 farms and 1985 household plots located in various soil and climatic zones of over 20,675 hectares in Central Asia. The materials were collected in the autumn (September-October), spring (April-May) and summer (June-August) months in 1970–1990 by the route method. Study subjects were plant parasitic nematodes of 8 species of wild and cultivated subtropical

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Rakic, Tamara, Jasmina Sinzar-Sekulic, Biljana Filipovic, Vanja Tadic, Branka Stevanovic, and Kit Tan. "Ecophysiological and anatomical characteristics of the subtropical shrub Zanthoxylum acanthopodium (Rutaceae) in conditions of a temperate continental climate (Serbia)." Archives of Biological Sciences 61, no. 2 (2009): 249–60. http://dx.doi.org/10.2298/abs0902249r.

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The evergreen shrub Zanthoxylum acanthopodium DC. (Rutaceae), originating from warm temperate and subtropical Asia, has existed successfully in the Jevremovac Botanical Garden in Belgrade for more than 80 years. The seasonal pattern of water management in leaves, electrolyte leakage, essential oil composition, and leaf anatomy were examined in order to understand the resistance and viability of this subtropical shrub in the temperate continental climate of Belgrade, Serbia.

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Krüger, K., U. Langematz, J. L. Grenfell, and K. Labitzke. "Climatological features of stratospheric streamers in the FUB-CMAM with increased horizontal resolution." Atmospheric Chemistry and Physics Discussions 4, no. 5 (2004): 6789–822. http://dx.doi.org/10.5194/acpd-4-6789-2004.

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Abstract. The purpose of this study is to investigate horizontal transport processes in the winter stratosphere using data with a high spatial and temporal resolution. For this reason the Freie Universität Berlin Climate Middle Atmosphere Model (FUB-CMAM) with its model top at 83 km altitude, increased horizontal resolution T42 and the semi-Lagrangian transport scheme for advecting passive tracers is used. A new result of this paper is the classification of specific transport phenomena within the stratosphere into tropical-subtropical streamer (e.g. Offermann et al., 1999) and polar vortex ext

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Wu, Zhiwei, Xinxin Li, Yanjie Li, and Yun Li. "Potential Influence of Arctic Sea Ice to the Interannual Variations of East Asian Spring Precipitation*." Journal of Climate 29, no. 8 (2016): 2797–813. http://dx.doi.org/10.1175/jcli-d-15-0128.1.

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Abstract Arctic sea ice (ASI) and its potential climatic impacts have received increasing attention during the past decades, yet the relevant mechanisms are far from being understood, particularly how anomalous ASI affects climate in midlatitudes. The spring precipitation takes up as much as 30% of the annual total and significantly influences agriculture in East Asia. Here, observed evidence and numerical experiment results show that the ASI variability in the Norwegian Sea and the Barents Sea in the preceding winter is intimately connected with interannual variations of the East Asian spring

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GOCHAKOV, A. V., O. YU ANTOKHINA, V. N. KRUPCHATNIKOV, and YU V. MARTYNOVA. "LONG-TERM VARIABILITY OF ROSSBY WAVE BREAKING IN THE SUBTROPICAL JET STREAM AREA." Meteorologiya i Gidrologiya, no. 2 (February 2022): 5–19. http://dx.doi.org/10.52002/0130-2906-2022-2-5-19.

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Climatology and variability of anticyclonic (AC-type) and cyclonic (C-type) wave breaking in the region of the subtropical jet stream are investigated using the previously developed method for identifying and clustering Rossby wave breaking events. Potential vorticity at an isentropic surface of 350 K from the ERA-Interim and ERA5 reanalyses are used. The results of applying the methods for the two reanalyses are similar. However, there is a high inconsistency for cyclonic wave breaking events, especially in summer. The maximum for both types of wave breaking is registered in summer. There are

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Sun, Chunling, Hong Zhang, Lu Xu, et al. "Twenty-meter annual paddy rice area map for mainland Southeast Asia using Sentinel-1 synthetic-aperture-radar data." Earth System Science Data 15, no. 4 (2023): 1501–20. http://dx.doi.org/10.5194/essd-15-1501-2023.

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Abstract. Over 90 % of the world's rice is produced in the Asia–Pacific region. Synthetic-aperture radar (SAR) enables all-day and all-weather observations of rice distribution in tropical and subtropical regions. The complexity of rice cultivation patterns in tropical and subtropical regions makes it difficult to construct a representative data-relevant rice crop model, increasing the difficulty in extracting rice distributions from SAR data. To address this problem, a rice area mapping method for large regional tropical or subtropical areas based on time-series Sentinel-1 SAR data is propose

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Liu, Yi, Yuli Zhang, Yong Wang, et al. "Dominant Modes of Tropospheric Ozone Variation over East Asia from GOME Observations." Advances in Meteorology 2015 (2015): 1–10. http://dx.doi.org/10.1155/2015/879578.

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The variation in tropospheric ozone over East Asia was analyzed using tropospheric column ozone data measured by the Global Ozone Monitoring Experiment (GOME) satellite. An empirical orthogonal function (EOF) analysis was carried out to derive the dominant modes of the variation in the tropospheric ozone volume-mixing ratio (TOVMR). The EOF1 mode, which explained 61.5% of the total variance, showed a same-sign distribution over all of East Asia, with a belt of enhanced ozone concentrations around 40°N. The principal component of EOF1 (PC1) suggested that photochemical ozone production together

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Rasyid, Sri Anggarini, Sugireng, Nurnaningsih, Sanatang, and Suwarny. "Dengue Virus Detection in Dengue Hemorrhagic Fever Patients Using the NS1 Antigen-Based Test with Immunochromatography and SDS-Page Methods in the Regional General Hospital of Kendari City." Journal of Biomimetics, Biomaterials and Biomedical Engineering 55 (March 28, 2022): 3–10. http://dx.doi.org/10.4028/p-3zkax3.

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Dengue Hemorrhagic Fever is one of the diseases that widely damages people; this disease is always found in tropical and subtropical regions, especially in Southeast Asia, Africa, and North Amerika [1]

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Stephan, Claudia Christine, Nicholas P. Klingaman, and Andrew G. Turner. "A Mechanism for the Recently Increased Interdecadal Variability of the Silk Road Pattern." Journal of Climate 32, no. 3 (2019): 717–36. http://dx.doi.org/10.1175/jcli-d-18-0405.1.

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The Silk Road pattern (SRP) teleconnection manifests in summer over Eurasia, where it is associated with substantial temperature and precipitation anomalies. The SRP varies on interannual and decadal scales; reanalyses show an increase in its decadal variability around the mid-1970s. Understanding what drives this decadal variability is particularly important, because contemporary seasonal prediction models struggle to predict the phase of the SRP. Based on analysis of observations and multiple targeted numerical experiments, this study proposes a mechanism for decadal SRP variability. Causal

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Li, Xinyu, and Riyu Lu. "Breakdown of the Summertime Meridional Teleconnection Pattern over the Western North Pacific and East Asia since the Early 2000s." Journal of Climate 33, no. 19 (2020): 8487–505. http://dx.doi.org/10.1175/jcli-d-19-0746.1.

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AbstractThe meridional teleconnection over the western North Pacific and East Asia (WNP–EA) plays a predominant role in affecting the interannual variability of East Asian climate in summer. This study identified a breakdown of the meridional teleconnection since the early 2000s. Before the early 2000s, there are close tropical–extratropical relationships in light of both circulation and rainfall anomalies. For instance, the westward extension of the western North Pacific subtropical high (WNPSH) is closely associated with the southward shift of the East Asian westerly jet (EAJ), and more rain

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Mao, Fangjie, Xuejian Li, Guomo Zhou, et al. "Land use and cover in subtropical East Asia and Southeast Asia from 1700 to 2018." Global and Planetary Change 226 (July 2023): 104157. http://dx.doi.org/10.1016/j.gloplacha.2023.104157.

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Zou, Xuxin, Li Yan, Jianjun Xu, and Shaojun Zheng. "The Impacts of Regime Shift in Summer Arctic Oscillation on Precipitation in East Asia." Atmosphere 15, no. 3 (2024): 283. http://dx.doi.org/10.3390/atmos15030283.

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Using multiple observational and reanalysis data, this paper investigates the impact of the interdecadal shift in summer Arctic Oscillation (AO) on precipitation in East Asia, by removing ENSO influences. The results indicate that the lower-layer activity center of summer AO in Atlantic shifted eastward after the mid-1980s. This regime shift of summer AO has a significant impact on precipitation in East Asia. Before the mid-1980s, the key regions in which precipitation was affected by AO in East Asia were northern East Asia and Northeastern China and adjacent regions. After the mid-1980s, the

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Xu, Hongna, Tao Wang, and Huijun Wang. "The Interdecadal Pacific Oscillation is responsible for the linkage of decadal changes in precipitation and moisture in arid central Asia and the humid Asian monsoon region during the last millennium." Climate of the Past 20, no. 1 (2024): 107–19. http://dx.doi.org/10.5194/cp-20-107-2024.

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Abstract. Reconstruction and observational studies imply a potential linkage of moisture and precipitation change in arid central Asia and monsoonal East Asia, in which the evolution of moisture and precipitation in central Asia is out of phase with that in northern China but in phase with that in southern China. In order to ascertain whether there is a robust linkage between the changes in climate in Asian arid regions and monsoon regions and to elucidate the underlying dynamic mechanisms, we analyzed the Last Millennium Reanalysis dataset and outputs from the Community Earth System Model Las

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Liu, Jiawei, Haiming Xu, and Jiechun Deng. "Projections of East Asian summer monsoon change at global warming of 1.5 and 2 °C." Earth System Dynamics 9, no. 2 (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 r

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Mitra, S. K., D. Majhi, H. Lembisana Devi, and P. K. Pathak. "POTENTIAL UNDERUTILIZED TROPICAL AND SUBTROPICAL FRUITS OF ASIA AND OCEANIA." Acta Horticulturae, no. 921 (December 2011): 111–15. http://dx.doi.org/10.17660/actahortic.2011.921.13.

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Dasgupta, S. "Tropical and subtropical fruits in Asia: future prospects and limitations." Acta Horticulturae, no. 1186 (November 2017): 199–202. http://dx.doi.org/10.17660/actahortic.2017.1186.31.

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Liu, Yuzhi, Tianbin Shao, Shan Hua, Qingzhe Zhu, and Run Luo. "Association of anthropogenic aerosols with subtropical drought in East Asia." International Journal of Climatology 40, no. 7 (2019): 3500–3513. http://dx.doi.org/10.1002/joc.6410.

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Jiang, Jie, Tianjun Zhou, Hailong Wang, Yun Qian, David Noone, and Wenmin Man. "Tracking Moisture Sources of Precipitation over Central Asia: A Study Based on the Water-Source-Tagging Method." Journal of Climate 33, no. 23 (2020): 10339–55. http://dx.doi.org/10.1175/jcli-d-20-0169.1.

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AbstractCentral Asia is a semiarid to arid region that is sensitive to hydrological changes. We use the Community Atmosphere Model, version 5 (CAM5), equipped with a water-tagging capability, to investigate the major moisture sources for climatological precipitation and its long-term trends over central Asia. Europe, the North Atlantic Ocean, and local evaporation, which explain 33.2% ± 1.5%, 23.0% ± 2.5%, and 19.4% ± 2.2% of the precipitation, respectively, are identified as the most dominant moisture sources for northern central Asia (NCA). For precipitation over southern central Asia (SCA),

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Yuan, Weihua, Rucong Yu, Minghua Zhang, Wuyin Lin, Haoming Chen, and Jian Li. "Regimes of Diurnal Variation of Summer Rainfall over Subtropical East Asia." Journal of Climate 25, no. 9 (2012): 3307–20. http://dx.doi.org/10.1175/jcli-d-11-00288.1.

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Using hourly rain gauge records and Tropical Rainfall Measuring Mission 3B42 from 1998 to 2006, the authors present an analysis of the diurnal characteristics of summer rainfall over subtropical East Asia. The study shows that there are four different regimes of distinct diurnal variation of rainfall in both the rain gauge and the satellite data. They are located over the Tibetan Plateau with late-afternoon and midnight peaks, in the western China plain with midnight to early-morning peaks, in the eastern China plain with double peaks in late afternoon and early morning, and over the East Chin

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Yuan, Weihua, Rucong Yu, Minghua Zhang, Wuyin Lin, Jian Li, and Yunfei Fu. "Diurnal Cycle of Summer Precipitation over Subtropical East Asia in CAM5." Journal of Climate 26, no. 10 (2013): 3159–72. http://dx.doi.org/10.1175/jcli-d-12-00119.1.

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Abstract The simulations of summertime diurnal cycle of precipitation and low-level winds by the Community Atmosphere Model, version 5, are evaluated over subtropical East Asia. The evaluation reveals the physical cause of the observed diurnal rainfall variation in East Asia and points to the source of model strengths and weaknesses. Two model versions with horizontal resolutions of 2.8° and 0.5° are used. The models can reproduce the diurnal phase of large-scale winds over East Asia, with an enhanced low-level southwesterly in early morning. Correspondingly, models successfully simulated the

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Huang, Ronghui, Jingliang Huangfu, Yong Liu, and Riyu Lu. "The Guiding Role of Rossby Wave Energy Dispersion Theory for Studying East Asian Monsoon System Dynamics." Atmosphere 14, no. 6 (2023): 962. http://dx.doi.org/10.3390/atmos14060962.

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This paper is written to commemorate the 10th anniversary of academician Ye Duzheng (Yeh T.C.) pass away and his great contributions to the development of atmospheric dynamics. Under the inspiration and guidance of the theory of Rossby wave energy dispersion, remarkable progresses have been made in research on planetary wave dynamics and teleconnections of atmospheric circulation anomalies. This paper aims to make a brief review of the studies on the propagating characteristics of quasi-stationary planetary waves in a three-dimensional spherical atmosphere and the dynamic processes of the inte

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Eccles, Rohan, Hong Zhang, and David Hamilton. "A review of the effects of climate change on riverine flooding in subtropical and tropical regions." Journal of Water and Climate Change 10, no. 4 (2019): 687–707. http://dx.doi.org/10.2166/wcc.2019.175.

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Abstract Tropical and subtropical regions can be particularly severely affected by flooding. Climate change is expected to lead to more intense precipitation in many regions of the world, increasing the frequency and magnitude of flood events. This paper presents a review of studies assessing the impacts of climate change on riverine flooding in the world's tropical and subtropical regions. A systematic quantitative approach was used to evaluate the literature. The majority of studies reported increases in flooding under climate change, with the most consistent increases predicted for South As

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