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首页> 外文期刊>International Journal of Biometeorology: Journal of the International Society of Biometeorology >Spatiotemporal variations of the start of thermal growing season for grassland on the Qinghai-Tibetan Plateau during 1961-2014
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Spatiotemporal variations of the start of thermal growing season for grassland on the Qinghai-Tibetan Plateau during 1961-2014

机译:青藏高原1961 - 2014年青藏高原热产生长季节开始时的时空变化

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摘要

The start of thermal growing season (STGS) is an important indicator for climate change effects on regional plant growth and development. This study comprehensively investigated and compared the spatiotemporal variations in STGS at 0 degrees C (STGS_0), 5 degrees C (STGS_5), and 10 degrees C (STGS_10) thresholds for grassland on the Qinghai-Tibetan Plateau (QTP) during 1961-2014. Although elevation was the predominant influencing factor of the spatial variations of STGSs, the effect of latitude should not be ignored at the low-elevation regions, especially for the STGS with a low-temperature threshold (e.g., STGS_0). With the decrease of temperature thresholds, the effect of elevation became weaker, while the effect of latitude became stronger. Significant advancing trends were observed in all the three STGSs, with greater advancing rate for STGS_0 (0.23daysyear(-1)) than that of STGS_5 (0.15daysyear(-1)) and STGS_10 (0.16daysyear(-1)). More obvious advancing trends were found after 1980, which coincided with more rapid climate warming. The advancing trends weakened after 1998 when climate warming hiatus occurred. Since positive and negative impacts may be simultaneously induced by the advanced STGSs, more observations are still needed to analyze their impacts on the growth and development of alpine grassland on the QTP.
机译:热生长季节(STG)的开始是气候变化对区域植物生长和发展影响的重要指标。本研究全面研究,并将STG的STG在0摄氏度(STGS_0),5摄氏度(STGS_5)和10摄氏度(STGS_10)和10摄氏度(QTP)上的10摄氏度(STGS_10)阈值进行了比较了在1961 - 2014年期间的10摄氏度。虽然高程是STG的空间变化的主要影响因素,但纬度不应在低升高区域忽略纬度,特别是对于具有低温阈值的STG(例如,STGS_0)。随着温度阈值的降低,仰角的效果变弱,而纬度的效果变得更强。在所有三种STG中观察到显着的推进趋势,具有比STGS_0(0.23daysyear(-1))更高的推进率(0.23daysyear(-1))(0.15daysyear(-1))和STGS_10(0.16daysyear(-1))。 1980年以后发现了更明显的推进趋势,这与气候变暖恰逢其当。 1998年在气候变暖的突然发生时,促进趋势削弱了。由于可以通过先进的STG同时引起正负影响,因此仍然需要更多的观察来分析它们对QTP上高山草原的生长和发展的影响。

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