2013
DOI: 10.5194/hess-17-2501-2013
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Expected changes in future temperature extremes and their elevation dependency over the Yellow River source region

Abstract: Abstract. Using the Statistical DownScaling Model (SDSM) and the outputs from two global climate models, we investigate possible changes in mean and extreme temperature indices and their elevation dependency over the Yellow River source region for the two future periods 2046-2065 and 2081-2100 under the IPCC SRES A2, A1B and B1 emission scenarios. Changes in interannual variability of mean and extreme temperature indices are also analyzed. The validation results show that SDSM performs better in reproducing th… Show more

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Cited by 17 publications
(9 citation statements)
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References 53 publications
(73 reference statements)
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“…The global average temperature has increased by about 0.13°C per decade since 1950 (IPCC 2007a). Significant warming trends in the Himalayan and Tibetan regions, generally higher than the global average, are reported in the literature (Shrestha et al 1999;Hu et al 2011Hu et al , 2013. Furthermore, the rate of warming is generally larger at the higher elevation (Sharma et al 2009;Hu et al 2013).…”
Section: Introductionsupporting
confidence: 48%
See 1 more Smart Citation
“…The global average temperature has increased by about 0.13°C per decade since 1950 (IPCC 2007a). Significant warming trends in the Himalayan and Tibetan regions, generally higher than the global average, are reported in the literature (Shrestha et al 1999;Hu et al 2011Hu et al , 2013. Furthermore, the rate of warming is generally larger at the higher elevation (Sharma et al 2009;Hu et al 2013).…”
Section: Introductionsupporting
confidence: 48%
“…Significant warming trends in the Himalayan and Tibetan regions, generally higher than the global average, are reported in the literature (Shrestha et al 1999;Hu et al 2011Hu et al , 2013. Furthermore, the rate of warming is generally larger at the higher elevation (Sharma et al 2009;Hu et al 2013). Such warming trends in the world's largest and highest mountain system will obviously influence the glacier and snow dynamics, leading to changes in water resources availability, particularly during spring and autumn ).…”
Section: Introductionmentioning
confidence: 67%
“…Researchers pointed out that precipitation in the wet season (June-September) is caused by the southwest monsoon from the Bay of Bengal in the Indian Ocean, that is, the Indian Summer Monsoon (Hu, Maskey, & Uhlenbrook, 2013a;Hu, Maskey, Uhlenbrook, & Zhao, 2011;Zheng et al, 2009). However, other researchers pointed out that the climate in the Yellow River source region is strongly governed by the East Asian Summer Monsoon, which brings warm and wet air in the summer (Hu, Maskey, & Uhlenbrook, 2013b;Lan et al, 2010b;Yang, Ding, Chen, Liu, & Lu, 2003). Based on the previous studies, the Yellow River source region is both the maximum northward extent of the Indian Summer Monsoon (Tian et al, 2007;Yao et al, 2009) and the maximum westward extent of the East Asian Summer Monsoon (Araguás-Araguás et al, 1998;Johnson & Ingram, 2004).…”
mentioning
confidence: 99%
“…One of the major climatic factor responsible for agricultural production is temperature (both maximum and minimum). According to IPCC 2007 the global average temperature has gone up by about 0.13 0 C per decade since 1950 .The study suggests that warming trends in the Himalayan region and nearby is significant, generally higher compared to global average (Shrestha et al 1999;Hu et al2011Hu et al , 2013. The study also suggests that the rate of warming is most often increases with increased elevation (Sharma et al 2009;Hu et al2013).…”
Section: Introductionmentioning
confidence: 98%