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Comment on Wood et al. 2008, 'Impacts of fire on forest age and runoff in mountain ash forests'

机译:评论Wood等。 2008年,“火灾对山灰森林的森林年龄和径流的影响”

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摘要

Wood et al. (2008; FPB 35) concluded their measurements of evapotranspiration (ET) in Eucalyptus regnans F.Muell. forest at Wallaby Creek, Victoria showed that ET differs only slightly between regrowth and oldgrowth, contrary to the findings of previous research. We assert that the conclusions of Wood et al. are invalid and argue that Wood et al. substantially overestimated annual transpiration and rainfall. Monthly whole-forest ET measured by Wood et al. using eddy covariance in a 296-year-old stand sum to ~700 mm year⁻¹; consistent with rainfall of 721 mm year⁻¹ recorded nearby by the Bureau of Meteorology. However, the Wood et al. conclusions were based on 1077 mm annual transpiration at this site, which appears to be estimated from a few months of heat pulse velocity measurements. Transpiration alone cannot be 54% higher than whole-forest ET because the latter includes transpiration, rainfall interception and evaporation from the forest floor. We believe Wood et al. made errors in scaling heat pulse velocities to whole-stand annual transpiration. Their rainfall of 1175 mm year⁻¹ averages 62% higher than at three Bureau of Meteorology and Melbourne Water sites nearby. The paper also contains inaccuracies in reporting of the literature and numerous other errors.
机译:伍德等。 (2008年; FPB 35)总结了他们对桉树F.Muell的蒸散量(ET)的测量结果。维多利亚州Wallaby Creek的森林表明,ET和再生植物之间仅存在细微的差异,这与之前的研究结果相反。我们断言伍德等人的结论。是无效的,并认为伍德等人。大大高估了年蒸腾量和降雨量。 Wood等人测得的每月全林ET。在296年历史的机架总和中使用涡流协方差,年限约为700毫米¹¹;符合气象局附近记录的721毫米1年的降水量¹。然而,伍德等。结论是基于该地点1077 mm的年蒸腾量,这似乎是根据几个月的热脉冲速度测量估算得出的。仅蒸腾作用不能比整个森林的ET高54%,因为后者包括蒸腾作用,降雨拦截和林地蒸发。我们相信伍德等人。在按比例缩放热脉冲速度以实现全年站立蒸腾方面存在错误。他们的1175毫米年⁻¹的降雨量比附近三个气象局和墨尔本水利站点的平均降雨量高62%。本文还包含不准确的文献报道和许多其他错误。

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