首页> 外文期刊>International Journal of Biometeorology: Journal of the International Society of Biometeorology >Inter-annual variation in the response of leaf-out onset to soil moisture increase in a teak plantation in northern Thailand
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Inter-annual variation in the response of leaf-out onset to soil moisture increase in a teak plantation in northern Thailand

机译:泰国北部柚木园人工林出苗对土壤水分增加的年际变化

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摘要

To understand the impact of inter-annual climate change on vegetation-atmosphere mass and energy exchanges, it has become necessary to explore changes in leaf-out onset in response to climatic fluctuations. We examined the response of leaf-out and transpiration onset dates to soil moisture in a teak plantation in northern Thailand based on a 12-year leaf area index and sap flow measurements. The date of leaf-out and transpiration onset varied between years by up to 40 days, and depended on the initial date when the relative extractable water in a soil layer of 0-0.6 m (Theta) was greater than 0.2 being consistent with our previous results. Our new finding is that the delay in leaf-out and transpiration onset relative to the initial date when Theta>0.2 increases linearly as the initial date on which Theta>0.2 becomes earlier. The delay spans about 20 days in years when Theta>0.2 occurs in March (the late dry season)-much earlier than usual because of heavy pre-monsoon rainfalls-while there is little delay in years when Theta>0.2 occurs in May. This delay indicates the influence of additional factors on leaf-out onset, which controls the delay in the response of leaf-out to soil moisture increase. The results increased our knowledge about the pattern and extent of the changes in leaf phenology that occur in response to the inter-annual climate variation in tropical regions, where, in particular, such research is needed
机译:为了了解年际气候变化对植被-大气质量和能量交换的影响,有必要探索应对气候波动的叶期开始变化。我们根据12年叶面积指数和树液流量测量结果,研究了泰国北部柚木种植园中叶期和蒸腾开始日期对土壤水分的响应。每年的出叶和蒸腾日期最多相隔40天,这取决于初始日期(当土壤层中0-0.6 m(Theta)的相对可提取水大于0.2时,与我们之前的一致)。结果。我们的新发现是,当Theta> 0.2变得更早时,相对于初始日期(当Theta> 0.2时呈线性增加),叶期和蒸腾开始的延迟相对于初始日期有所延迟。在3月(干旱后期),Theta> 0.2发生的年份中,延迟时间跨度约为20天-由于季风前的大雨比平常早得多-而在5月,Theta> 0.2发生的年份几乎没有延迟。该延迟表明了其他因素对叶面开始的影响,该因素控制叶面对土壤水分增加的响应的延迟。结果增加了我们对响应热带地区年际气候变化而发生的叶片物候变化的模式和程度的了解,尤其是在需要进行此类研究的情况下

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