Evolution and correlation characteristics of wire and ice layer temperatures under different weather conditions in the mountainous regions of Southwestern China
摘要
Different from the air temperature, the wire temperature is not only affected by the meteorological conditions, but also can directly reflect some important characteristics of the icing process, which is the basis for judging the dry and wet growth of ice accretion. Based on the comprehensive observations to air temperature (Ta), wire temperature measured directly (Twd) and by infrared radiation (Twi) over the winters from 2019 to 2021 in the southwestern mountainous areas of China, this study combines the three-types temperature under different weather conditions to reveal the response characteristics of wire temperature to the icing processes. The results show that solar shortwave radiation has the most significant impact on wire temperature, but exhibits different characteristics under diverse weather conditions. Among them, Twd is significantly higher than Ta during the daytime of sunny days, while during the nighttime of rainy/foggy days, the values of these two temperatures are closest. Compare to Ta, Twd and Twi can effectively reveal that the most prominent disaster characteristics of ice accretion. Twd and Twi exhibited a strong positive correlation during the icing process, particularly at night. An ice weight growth rate exceeding 15 g/h occurred mainly when Twd or Twi ranged from − 2.5 °C to 0 °C. Twd is greater than 0 °C during the daytime can well interpret the occurrence of ice shedding when Ta is less than 0 °C. There is the wet growth process of ice accretion with a Twi of 0 °C during the daytime, while it is dominated by the dry growth process of ice accretion with Twi below 0 °C during the nighttime. The energy balance method can be applied to estimate the wire temperature, especially during the icing processes when the wire temperature is less than 0 ℃.