Inter-hemispheric comparison of climate change in the last millennium based on the ECHO-G simulation

Kuang, Xueyuan; Liu, Jian; Wang, Hongli; Wang, Sumin

doi:10.1007/s11434-008-0193-9

Cited by 3 publications

(2 citation statements)

References 38 publications

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“…The long-term mean annual temperature (T annual ) used as evidence of regional climate change record in this study, was reconstructed using the ECHO-G model (Kuang et al, 2008) and based on the instrumental data starting from 1960 from the nearby meteorological station and therefore extend the time series of regional temperature back to ca. 1800 AD (Fig.…”

Section: Study Sitementioning

confidence: 99%

The response of Cladocerans to recent environmental forcing in an Alpine Lake on the SE Tibetan Plateau

et al. 2016

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Section: Study Sitementioning

confidence: 99%

The response of Cladocerans to recent environmental forcing in an Alpine Lake on the SE Tibetan Plateau

et al. 2016

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“…The variability of the global [26] and East Asian [27] summer monsoon precipitation, as well as the inter-hemispheric comparison of climate change [28] during the last millennium has also been studied. Here, our focus is summer climate change on centennial time scale in eastern China, including the mechanistic basis of such changes.…”

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confidence: 99%

Simulated analysis of summer climate on centennial time scale in eastern China during the last millennium

et al. 2011

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Using Lanczos filtered simulation results from the ECHO-G coupled ocean-atmosphere model, this study analyzes the spatiotemporal structure of temperature and precipitation on centennial time scale to examine how climate change in eastern China responded to external forcing during the last millennium. The conclusions are (1) eastern China experienced a warm-cold-warm climate transition, and the transition from the warm period to the cold period was slower than the cold to warm transition which followed it. There was more rainfall in the warm periods, and the transitional peak and valley of precipitation lag those of temperature. The effective solar radiation and solar irradiance have significant impacts on the temporal variation of both temperature and precipitation. Volcanic activity plays an important role in the sudden drop of temperature before the Present Warm Period (PWP). There is a positive correlation between precipitation and volcanic activity before 1400 A.D., and a negative relationship between the two thereafter. The concentration of greenhouse gases increases in the PWP, and the temperature and precipitation increase accordingly. (2) The spatial pattern of the first leading empirical orthogonal function (EOF) mode of temperature on centennial time scale is consistent with that on the inter-annual/inter-decadal (IA-ID) time scales; namely, the entirety of eastern China is of the same sign. This pattern has good coherence with effective solar radiation and the concentrations of greenhouse gases. The first leading EOF mode of precipitation on centennial time scale is totally different from that on the IA-ID time scales. The first leading mode of centennial time scale changes consistently over the entirety of eastern China, while the middle and lower reaches of the Yangtze and Yellow Rivers are the opposite to the rest of eastern China is the leading spatial pattern on IA-ID time scale. The distribution of precipitation on centennial time scale is affected by solar irradiance and greenhouse gas concentrations.

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Interactive effects of climate-atmospheric cycling on aquatic communities and ecosystem shifts in mountain lakes of southeastern Tibetan Plateau

Wang,

Yang

et al. 2024

Science of The Total Environment

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Inter-hemispheric comparison of climate change in the last millennium based on the ECHO-G simulation

Cited by 3 publications

References 38 publications

The response of Cladocerans to recent environmental forcing in an Alpine Lake on the SE Tibetan Plateau

The response of Cladocerans to recent environmental forcing in an Alpine Lake on the SE Tibetan Plateau

Simulated analysis of summer climate on centennial time scale in eastern China during the last millennium

Interactive effects of climate-atmospheric cycling on aquatic communities and ecosystem shifts in mountain lakes of southeastern Tibetan Plateau

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