Impact of the Return Flow on Heavy Pollution in Winter over the Beijing–Tianjin–Hebei Region

Mei, Mei; Wang, Zunya

doi:10.1007/s13351-023-2141-7

Cited by 4 publications

(1 citation statement)

References 47 publications

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“…The western coast of the Bohai Sea represents a typical "C"-shaped coastal zone. The unique geographical environment results in frequent occurrences of dense fog, which are often associated with easterly winds passing over the Bohai Sea [10]. Ye et al [11] categorized the weather patterns in North China into nine classes using T-type rotated principal component analysis (T-PCA).…”

Section: Introductionmentioning

confidence: 99%

Impact of the Sea Effect on Sudden Fog on the Western Coast of the Bohai Sea: A Case Study

Tian,

Wu,

Wang

et al. 2024

Atmosphere

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The term “sea effect” generally refers to the process of air mass modification after cold air flows above a warm sea surface. Affected by the sea effect, small-scale and sudden fogs have occasionally been observed on the western coast of the Bohai Sea. A more in-depth study of this type of fog is crucial for ensuring the safety of maritime and aerial traffic routes in this region. This study investigated the formation mechanism of this specific type of fog on the morning of 17 October 2007, utilizing both meteorological stations and 255 m tower observations, combined with the results of the Weather Research and Forecasting model (WRF). It is demonstrated that Bohai Sea evaporation and the associated water vapor advection played crucial roles in the formation of fog along the west coast of the Bohai Sea. The cold return flow became more moist as it passed over the warm Bohai Sea, which was the primary contributor to triggering regional fog on the western coast. A moisture budget analysis revealed that water vapor from the Bohai Sea intruded into its western coast along an eastward trajectory, dominating the oscillations in the net moisture flux. The eastern water vapor flux significantly increased at 17:00 on the 16th (Local time, LST), reaching its peak at 21:00. Correspondingly, the fog water growth rate began to increase at 23:00 on the 16th, reaching its maximum at 03:00 on the 17th. A sensitivity experiment on evaporation further indicated that the Bohai sea effect played a decisive role in fog formation. With a tenfold reduction in evaporation from the Bohai Sea and subsequent significant weakening of water vapor advection, the simulated fog along the western coast of the Bohai Sea completely disappeared. Understanding the formation mechanism of this type of fog is beneficial for refining forecasting focal points, thereby enhancing forecast accuracy in a targeted manner.

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Section: Introductionmentioning

confidence: 99%