Abstract
Yunnan–Guizhou quasi-stationary front (YGQSF) is a unique weather phenomenon that frequently occurs during the winter half year over the Yunnan–Guizhou Plateau in southwestern China. Most of the previous studies analyzed it only with synoptic cases. This study investigates the structure, variation, and impact of this front from a climate perspective, using long-term high-resolution atmospheric reanalyses and high-density station records for 1981–2016. An objective method quantifying YGQSF is proposed and three indexes are defined to measure its intensity, frequency, and location, respectively, with horizontal gradient of air potential temperature at a terrain-following level of sigma 0.995. With these indexes, climatological structure, subseasonal variability as well as climatic impact of the front are comprehensively examined. In climatology, YGQSF as a north–south-oriented low-level front is found to occur the most frequently during January–February–March, determined predominately by the coldness from the east of the front. The structure of the front identified essentially reflects an obstruction of high-terrain Yunnan (the western part of the plateau) to the low-level cold air mass, which makes near-surface cold northeasterly winds cease westward intruding and veer upward over relatively low-terrain Guizhou, transporting moisture upward and forming low clouds. A sharp climate contrast is thus formed between two sides of the front: cold, sunless, and continuously rainy Guizhou versus warm and sunny Yunnan. Furthermore, the front features significant subseasonal variations with periods at around 30 days and 60 days largely in its intensity. Anomalously strong YGQSF events which are caused 75% by the cold anomaly from the east but no more than 17% by the warm anomaly from the west yield different anomalous structures, but consistently amplify the sharp climate contrast between Yunnan and Guizhou.
Highlights
The quasi-stationary front is a unique weather phenomenon that frequently occurs during the winter half year in southwestern China
Since this front is found to be always anchored in the Yunnan–Guizhou Plateau, a specific region with the Tibetan Plateau on its northwestern side and vast plains and hills on its eastern side (Fig. 1), it is usually referred to as the Yunnan–Guizhou quasi-stationary front (YGQSF)
In order to comprehensively capture the general characteristics of YGQSF, it is necessary to conduct the investigation from a climate perspective
Summary
Based on the thermodynamic method proposed by Hewson (1998), Zhao et al (2019) recognized three YGQSF events occurring at 850 hPa in early 2008, it is difficult to recognize a low-level front over the complex terrain (Jenkner et al 2010). This study defines three indexes to quantitatively characterize YGQSF based on both topographic features of Yunnan–Guizhou Plateau and objective criteria. With these quantified indexes, the climatological structure, the subseasonal variability as well as the climatic impact of YGQSF are examined with longterm high-resolution atmospheric reanalysis data and observations from high-density stations. A climate perspective of the quasi‐stationary front in southwestern China: structure, variation
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