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首页> 外文期刊>Agricultural and Forest Meteorology >Influences of temperature and precipitation before the growing season on spring phenology in grasslands of the central and eastern Qinghai-Tibetan Plateau.
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Influences of temperature and precipitation before the growing season on spring phenology in grasslands of the central and eastern Qinghai-Tibetan Plateau.

机译:青藏高原中部和东部高原生长期前的温度和降水对春季物候的影响。

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摘要

Spatial variations in phenological responses to temperature have not been reported for grasslands of the Qinghai-Tibetan Plateau. Using satellite-derived normalized difference vegetation index and meteorological records from 1982 to 2006, we characterized the spatial patterns of grassland green-up onset in relation to air temperature and precipitation before the growing season ("preseason" henceforth) in the central and eastern plateau by combining linear programming with correlation analysis. Green-up onset near half of the meteorological stations was significantly correlated (p<0.10) with precipitation and thermal spring onset (TSO) date based on the cumulative temperature less than 6 weeks before the onset. The green-up onset paralleled the advance in TSO in the southwestern, southeastern, eastern, and northeastern parts of the plateau. The TSO and preseason precipitation (PPT) explained part of the inter-annual phenological variations, with r2 varying between 0.05 and 0.55 and averaging 0.28, and did not explain delay of green-up onset in some areas. Increasing preseason temperature tended to advance green-up onset in relatively moist areas. PPT exerted a stronger influence on green-up onset in drier areas. These results indicate spatial differences in the key environmental influences on spring phenology. To improve the ability to predict onset, ground-based community-level phenological studies and spatial scaling-up of the phenology-climate relationship will be necessary.
机译:对于青藏高原的草原,尚未有对温度的物候响应的空间变化的报道。利用卫星归一化差异植被指数和1982-2006年的气象记录,我们对高原中部和东部高原生长期(此后的“季前”)之前草地绿化爆发的空间格局与气温和降水的关系进行了描述。通过将线性规划与相关分析相结合。基于累计温度低于6,近一半气象站的绿化发作与降水和热泉发作日期( p <0.10)显着相关( p <0.10)发病前几周。在高原的西南部,东南部,东部和东北部,绿色爆发与 TSO 的上升平行。 TSO 和季前降水( PPT )解释了年际物候变化的一部分,其中 r 2 变化在0.05到0.55之间,平均为0.28,并且不能解释某些地区的绿色发作延迟。季前温度升高往往会在相对潮湿的地区加剧绿化现象。 PPT 对较干燥地区的绿起病影响更大。这些结果表明对春季物候的关键环境影响的空间差异。为了提高预测发病的能力,有必要进行基于地面的社区一级物候研究,以及物候-气候关系的空间扩展。

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