Figure 1a shows that the maximum value of autumn precipitation is located over west china, with the total precipitation exceeding 300 mm throughout the fall in the center of the region thus, we define the autumn precipitation averaged over west china (27°–35°n, 100°–112°e) as a representative index for expressing wcap variability. Interannual to inter-decadal variability in the community of east asian monsoon studies, a sive rainfall in south china along the yangtze river valley this . Decadal variation of summer precipitation over china and associated atmospheric circulation after the late 1990s zhiqing xu climate change research center, chinese academy of sciences, and . Yang f and lau k 2004 trend and variability of china precipitation in spring of the central-pacific el niño to the atlantic multi-decadal oscillation . Autumn precipitation over hainan island, china of decadal variability revealed from the ep–np pat-tern previous works (tourre and white 1997, zhang.
On the basis of the latest observational datasets, the inter-decadal changes of summer rainfall in east china in the past 50 years are analyzed using the lepage test the two traditional methods moving t-test and mann-kendall test are also performed on the rainfall data as a comparison results . The eof analysis of both observed data and simulated data shows that the major patterns of decadal variation of summer precipitation over eastern china are a dipole pattern divided by the huaihe river and a four zonal bands alternate with each other centered at south china, the yangtze river valley, north china plain and northeast china. Interannual-to-decadal variability and trends of sea level in the south china sea (scs) are studied using altimetric data during 1993-2012 and reconstructed sea level data from 1950-2009 the interannual variability shows a strong seasonality surface wind anomalies associated with el nio-southern . The following new findings have been highlighted: (1) one dominating mode of the inter‐decadal variability of the summer precipitation in china is the near‐80‐yr oscillation other modes of 12‐yr and 30–40‐yr oscillations also play an important role in affecting regional inter‐decadal variability.
Spatiotemporal variability of temperature and precipitation in gansu province (northwest china) during 1951–2015 annual and inter-decadal variability in the . Background decadal to interdecadal variability of the climate over the south china sea regime shift of the climate over the south china sea millennium scale variability of the climate. Kairan ying, carsten s frederiksen, xiaogu zheng, jiale lou and tianbao zhao, variability and predictability of decadal mean temperature and precipitation over china in the ccsm4 last millennium simulation, climate dynamics, (2018). The present article is the second part of a study on the inter‐decadal variability of the summer precipitation in east china, which mainly addresses the possible cause of this change.
Decadal summer drought frequency in china: the increasing influence of the atlantic multi-decadal oscillation and variability of china precipitation in . Solar cycle signature in decadal variability of monsoon precipitation in china liang zhao, jingsong wang and haijuan zhao national satellite meteorological center, china meteorological . Introduction china is located in the east asian monsoon region, the variations of the amount and distribution of precipitation over china are strongly modulated by the east asian monsoon.
Centennial- to decadal-scale monsoon precipitation variability in the semi-humid region, northern china during the last 1860 years: records from stalagmites in huangye cave. Decadal (7- yr period) variations of precipitation over western north america account for 20%–50% of the variance of annual precipitation spatially, the decadal variability is broken into several regional [o(1000 km)]. The modes of variability that arise from the slow-decadal (potentially predictable) and intra-decadal (unpredictable) components of decadal mean temperature and precipitation over china are examined, in a 1000 year (850–1850 ad) experiment using the ccsm4 model solar variations, volcanic . Summer precipitation anomalies can lead to drought and flooding which have significant influence on society and economy of china, so it's important to understand the decadal variation of summer precipitation over china.
In east asia and winter precipitation over southern china after 1980 key words: east asian winter monsoon, winter precipitation, el ni˜no and la ni˜na, asymmetry, decadal variability. Decadal variability of the summer precipitation in china is the near-80-yr oscillation other modes of 12-yr and 30–40-yr oscillations also play an important role in affecting regional inter-decadal variability. Several decades that take into account both forced climate change and natural decadal-scale climate variability are in their infancy  many formidable .
Decadal variation of summer precipitation over china and associated atmospheric circulation after the late 1990s zhiqing xu and decadal variability with spatiotemporal structure,. Laboratory of climate studies, china meteorological administration, 46 zhongguancun nan da jie, haidian district, beijing 100081, china the present article is the second part of a study on the inter-decadal variability of the summer precipitation in east china, which mainly addresses the possible .
Decadal variability of summer rainfall over mainland china: observation vs a 1000-year simulation of hadcm3 yonghui lei1,2, brian hoskins 2,3 and julia slingo2,4 1state key laboratory of remote sensing science, institute of remote sensing. Interannual to decadal variability from longer term climate responses is essential for interpreting changes in the global water cycle (gu et al, 2016 sukhatme. The pacific decadal oscillation (pdo) is a robust, recurring pattern of ocean-atmosphere climate variability centered over the mid-latitude pacific basin the pdo is detected as warm or cool surface waters in the pacific ocean , north of 20°n.