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NOTES AND CORRESPONDENCE Inconsistencies in the 'New' Windchill Chart at Low Wind Speeds

机译:注意和对应“低风速”“新” Windchill图表中的不一致

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摘要

An apparent eiroi was detected in the calculation of windchill equivalent temperatures (WCETs) in the "new" chart and corresponding equation that were adopted in 2001 by the weather services in the United States and Canada. The problem is caused by significant discontinuities in WCETs at the assumed "calm" wind speed condition of 1.34 m s~(-1). As a result, published WCETs are not equal to, as they should be by definition, but are lower than air temperatures at the assumed calm wind speed condition.This inconsistency further propagates to higher wind speeds beyond the assumed calm condition. In this paper, a straightforward correction is proposed to circumvent these inconsistencies of the new windchill. The proposed correction makes this transition gradual rather than abrupt by applying it to the expression used for estimating the effects of wind on the convective heat exchange coefficient between humans and their cold and windy environment.
机译:在“新”图和2001年美国和加拿大的气象服务机构采用的相应方程式中的风冷等效温度(WCET)的计算中检测到明显的eiroi。该问题是由于在假设的“平静”风速条件为1.34 m s〜(-1)时WCET的明显不连续性引起的。结果,已发布的WCET并不等于定义上的平均值,而是低于假定的平静风速条件下的气温,这种不一致性进一步传播到了超出假定的平静条件下的更高风速。在本文中,提出了一种直接的纠正措施来规避新的Windchill的这些不一致之处。通过将其应用到用于估计风对人类及其寒冷多风环境之间对流热交换系数的影响的表达式,建议的校正使此过渡逐渐而不是突然地进行。

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