Abstract

ABSTRACT This study provides insight into how the visibility in Taiwan has varied over time and what the main drivers of these visibility changes are. From 1985 to 2016, urban inland sites showed increases in visibility and decreases in the frequency of hazy and/or foggy days, whereas urbanized and rural coastal regions either showed no clear trend or even an overall decrease in visibility. Over the most recent 5 to 10 years, a consistent increase in the visibility and decrease in the haze frequency has been found for most of the stations, except for the rural to suburban regions. In general, visibility is driven by the relative humidity (rH) and the mass concentration of aerosol particles (PM). On the one hand, the combination of climate change and urbanization, resulting in a rise in temperature (on average, +0.035°C y–1) and an associated overall decrease in rH (on average, –0.125% y–1), has had a positive influence on long-term visibility in the cities of Taiwan. On the other hand, improvements in air quality supported the increase in visibility during the late 2000s and early 2010s. Our results show an almost exponential relationship between visibility and PM10. At lower PM10 levels, the visibility is more sensitive to changes in the PM10. Thus, the influence of the long-term PM10 on visibility becomes weaker at high PM10 levels. Consequently, over the long term, the PM10 more strongly influenced the visibility trends at the northern urban stations, which had lower PM10 concentrations to begin with. At the southern urban stations, the PM10 concentrations were generally higher and hence were less of a factor in variations in visibility. Therefore, the visibility trends at these sites were more related to changes in rH until about 2011, at which time these regions reached a lower level of pollution.

Highlights

  • Both the scientific community and the public are concerned about atmospheric visibility

  • Depending on the ambient relative humidity (rH), haze refers to visibility reductions caused by dry particles, whereas mist refers to visibility reductions caused by wet hygroscopic particles or small water droplets (World Meteorological Organization, 2014, 2017)

  • There is no consistent pattern for all stations, we do see a consistent increase in visibility and decrease in the frequency of haze in the most recent 5 to 10 years at most of the stations, except for the rural to suburban regions of HC and MG

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Summary

Introduction

Both the scientific community and the public are concerned about atmospheric visibility. In accordance with the WMO’s definition (World Meteorological Organization, 2014, 2017), fog is described in the literature as a condition in the near-surface atmosphere when the relative humidity (rH) is near 100% and the horizontal visibility is reduced to less than 1 km due to the presence of small water droplets in the air. Depending on the ambient rH, haze refers to visibility reductions caused by dry particles, whereas mist refers to visibility reductions caused by wet hygroscopic particles or small water droplets (World Meteorological Organization, 2014, 2017). To differentiate between haze and mist, the WMO uses a threshold of relative humidity at 95% (World Meteorological Organization, 2014) or another “certain percentage” (e.g., 80%; World Meteorological Organization, 2017). Various studies have characterized haze and mist using different limits for the visibility range (e.g., Chung et al, 1999; Bruijnzeel et al, 2005; Vautard et al, 2009; Kuo et al, 2013; Akimoto and Kusaka, 2015), and the relative humidity level is often not even mentioned

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