1.1这些方法包括使用两种类型的气压计测量大气压力:Fortin型水银气压计和无液气压计。 1.2在没有异常扰动的情况下，在距离该点100 m的水平距离和0.5 m的垂直距离内，通过这些方法在该点测量的大气压力在任何地方都有效。 1.3大气压力随高度增加而降低，并随水平距离变化1 Pa/100 m或更小，除非发生灾难性现象（例如龙卷风）。因此，如果满足以下标准，则可以通过校正高度差来实现将已知大气压力扩展到1.2中规定的空间限制以外的另一个场地: 1.3.1新址横向2000米，纵向500米。 1.3.2前10分钟内的压力变化小于20 Pa。 压力， P 2. 位置2是已知压力的函数 P 1. 在站点1，海拔高度的代数差， h 1. − h 2. ，和之间空间中的平均绝对温度。之间的函数关系 P 1. 和 P 2. 如10.2所示。两者之间的区别 P 1. 和 P 2. 对于以下各项之间每1 m的差异: h 1. 和 h 2. 表1和10.4中给出了 P 1. 和平均温度。 1.4大气压力随时间变化。这些方法仅提供瞬时值。 1.5以国际单位制表示的数值应视为标准。 1.6 本标准并非旨在解决与其使用相关的所有安全问题（如有）。本标准的用户有责任在使用前制定适当的安全和健康实践，并确定监管限制的适用性。 第7节给出了具体的安全预防说明。 表1选定值 平均的 坦佩拉- 图雷 压力 P 1. 帕 110 000 100 000 90 000 80 000 70 000 更正为 P 1. ，Pa/m，如果为正 h 1. > h ，如果为负 h 1. < h 2. 230 16 15 13 12 10 240 16 14 13 11 10 250 15 14 12 11 10 260 14 13 12 11 9 270 14 13 11 10 9 280 13 12 11 10 9 290 13 12 11 9 8. 300 13 11 10 9 8. 310 12 11 10 9 8. ====意义和用途====== 大气压力是气象学家用来描述大气状态的基本变量之一。 当大气压力与 “ 标准 ” 在一些涉及压力因变量的科学和工程应用中，必须考虑压力条件。 这些方法提供了一种测量大气压力的方法，其精度和精密度可与政府气象机构的测量精度和精密度相媲美。

1.1 These methods cover the measurement of atmospheric pressure with two types of barometers: the Fortin-type mercurial barometer and the aneroid barometer. 1.2 In the absence of abnormal perturbations, atmospheric pressure measured by these methods at a point is valid everywhere within a horizontal distance of 100 m and a vertical distance of 0.5 m of the point. 1.3 Atmospheric pressure decreases with increasing height and varies with horizontal distance by 1 Pa/100 m or less except in the event of catastrophic phenomena (for example, tornadoes). Therefore, extension of a known barometric pressure to another site beyond the spatial limits stated in 1.2 can be accomplished by correction for height difference if the following criteria are met: 1.3.1 The new site is within 2000 m laterally and 500 m vertically. 1.3.2 The change of pressure during the previous 10 min has been less than 20 Pa. The pressure, P 2 at Site 2 is a function of the known pressure P 1 at Site 1, the algebraic difference in height above sea level, h 1 − h 2 , and the average absolute temperature in the space between. The functional relationship between P 1 and P 2 is shown in 10.2. The difference between P 1 and P 2 for each 1 m of difference between h 1 and h 2 is given in Table 1 and 10.4 for selected values of P 1 and average temperature. 1.4 Atmospheric pressure varies with time. These methods provide instantaneous values only. 1.5 The values stated in SI units are to be regarded as the standard. 1.6 This standard does not purport to address all of the safety concerns, if any, associated with its use. It is the responsibility of the user of this standard to establish appropriate safety and health practices and determine the applicability of regulatory limitations prior to use. Specific safety precautionary statements are given in Section 7. TABLE 1 Selected Values Average Tempera- ture, Pressure P 1 , Pa 110 000 100 000 90 000 80 000 70 000 Correction to P 1 , Pa/m, positive if h 1 > h , negative if h 1 < h 2 230 16 15 13 12 10 240 16 14 13 11 10 250 15 14 12 11 10 260 14 13 12 11 9 270 14 13 11 10 9 280 13 12 11 10 9 290 13 12 11 9 8 300 13 11 10 9 8 310 12 11 10 9 8 ====== Significance And Use ====== Atmospheric pressure is one of the basic variables used by meteorologists to describe the state of the atmosphere. The measurement of atmospheric pressure is needed when differences from “ standard ” pressure conditions must be accounted for in some scientific and engineering applications involving pressure dependent variables. These methods provide a means of measuring atmospheric pressure with the accuracy and precision comparable to the accuracy and precision of measurements made by governmental meteorological agencies.