Fig. 3: Reconstructed streamflow time series based on backward moving mean for the five gauging stations in headwater regions of major rivers in the South and East Tibetan Plateau (SETP). | Nature Communications

Fig. 3: Reconstructed streamflow time series based on backward moving mean for the five gauging stations in headwater regions of major rivers in the South and East Tibetan Plateau (SETP).

From: Reconstructed eight-century streamflow in the Tibetan Plateau reveals contrasting regional variability and strong nonstationarity

Fig. 3

a Tangnaihai (TNH, Yellow); b Zhimenda (ZMD, Yangtze); c Changdu (CD, Lancang-Mekong); d Jiayuqiao (JYQ, Nu-Salween); and e Nuxia (NX, Yarlung Zangbo-Brahmaputra). Black lines for all gauging stations represent time series of 52-year (33-year for JYQ) moving means for annual streamflow reconstructions. Grey lines represent 30-year moving averages. Buff bars show periods with statistically significant differences (p < 0.05) between the reconstructed streamflow within a 52-year (33-year for the JYQ) moving window and the observed streamflow (1961–2012) based on 2-sided t-test statistics. Values of the buff bars represent different significant levels but all p-values are lower than 0.05. Red dotted lines show the 95% confidence interval of mean values based on observed data. Blue dotted lines show the instrumental mean during 1961−2012 (1980−2012 for JYQ).

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