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Attribution of climate change: a methodology to estimate the potential contribution to increases in potato yield in Scotland since 1960.

机译:气候变化的归因:一种估算自1960年以来苏格兰马铃薯产量增加的潜在贡献的方法。

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Maincrop potato yields in Scotland have increased by 30-35 t ha-1 since 1960 as a result of many changes, but has changing climate contributed anything to this? The purpose of this work was to answer this question. Daily weather data for the period 1960-2006 were analysed for five locations covering the zones of potato growing on the east coast of Scotland (between 55.213 and 57.646 N) to determine trends in temperature, rainfall and solar radiation. A physiologically based potato yield model was validated using data obtained from a long-term field trial in eastern Scotland and then employed to simulate crop development and potential yield at each of the five sites. Over the 47 years, there were significant increases in annual air and 30 cm soil temperatures (0.27 and 0.30 K decade-1, respectively), but no significant changes in annual precipitation or in the timing of the last frost in spring and the first frost of autumn. There was no evidence of any north to south gradient of warming. Simulated emergence and canopy closure became earlier at all five sites over the period with the advance being greater in the north (3.7 and 3.6 days decade-1, respectively) than the south (0.5 and 0.8 days decade-1, respectively). Potential yield increased with time, generally reflecting the increased duration of the green canopy, at average rates of 2.8 t ha-1 decade-1 for chitted seed (sprouted prior to planting) and 2.5 t ha-1 decade-1 for unchitted seed. The measured warming could contribute potential yield increases of up to 13.2 t ha-1 for chitted potato (range 7.1-19.3 t ha-1) and 11.5 t ha-1 for unchitted potato (range 7.1-15.5 t ha-1) equivalent to 34-39% of the increased potential yield over the period or 23-26% of the increase in actual measured yields.Digital Object Identifier http://dx.doi.org/10.1111/j.1365-2486.2011.02601.x
机译:由于发生了许多变化,自1960年以来,苏格兰的主要农作物马铃薯产量增加了30-35 t ha -1 ,但是气候变化对此有何贡献?这项工作的目的是回答这个问题。对1960-2006年期间的每日天气数据进行了分析,以覆盖苏格兰东海岸的马铃薯种植区域(55.213至57.646 N)之间的五个位置,以确定温度,降雨量和太阳辐射的趋势。使用从苏格兰东部的长期田间试验获得的数据验证了基于生理的马铃薯产量模型,然后将其用于模拟五个地点中每个地点的作物生长和潜在产量。在这47年中,每年的空气温度和30 cm的土壤温度均显着增加(分别为0.27和0.30 K October -1 ),但年降水量或末次降水时间没有明显变化。春天的霜冻和秋天的霜冻。没有证据表明从北到南的变暖。在此期间内,所有五个地点的模拟出土和冠层关闭都变得更早,北部(分别为3.7和3.6天十年 -1 )的提前量大于南部(0.5和0.8天十年 sup> -1 )。杂种(播种前发芽)的潜在产量随时间增加,通常反映绿色树冠的持续时间增加,平均速率为2.8 t ha -1 十年 -1 )和2.5 t ha -1 十年 -1 的种子。测得的变暖可能会对马铃薯马铃薯(7.1-19.3 t ha -1 的范围)和11.5 t ha 的潜在产量增加高达13.2 t ha -1 未收割的马铃薯(范围为7.1-15.5 t ha -1 )为-1 ,相当于同期潜在产量增加的34-39%,或实际增加量的23-26%测量的产量数字对象标识符http://dx.doi.org/10.1111/j.1365-2486.2011.02601.x

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