Elevated Ducts and Low Clouds over the Central Western Pacific Ocean in Winter Based on GPS Soundings and Satellite Observation

• 作者: LI Xiaodong SHENG Lifang WANG Wencai
• 来源期刊: 中国海洋大学学报（自然科学英文版）
• 年，卷（期）: 2021,（2）
• 所属期刊栏目: Marine and Atmospheric Sciences
• 页码范围: 244-256
• 页数: 13页
• 语种: 英文

摘要

Both low clouds and elevated ducts are common phenomena in the oceanic atmosphere. Low clouds affect elevated ducts by changing the structure of atmospheric temperature and humidity. However, due to the limitation of met-ocean measurements, research on them is still scattered. This paper presents the distribution of elevated ducts and clouds over the central Western Pacific Ocean (WPO) based on Global Position System (GPS) sounding data and Himawari-8 satellite products from November 2015 to January 2016. Results show that the frequency of elevated ducts detected by ship-based GPS soundings was as high as 77％ over the central WPO. The height and frequency of elevated ducts are closely related to the low clouds. If there are no clouds, the occurrence probability and mean base height of the elevated ducts are 14％ and 730 m, respectively. By comparison, the occurrence probability and mean base height increase up to 24％ and 1471 m, respectively, in the presence of cumulus (Cu) clouds, and 22％ and 1511 m, respectively, in the presence of stratocumulus (Sc) clouds. Elevated ducts occur near the cloud top. The analysis of geopotential height and wind fields from the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis dataset (ERA-interim) shows that the study area is covered by a strong and stable subtropical high, and slowly sinking dry air masses inside the subtropical high are above the moist boundary-layer air mass. The appearance and evolution of low clouds will adjust the temperature and hu-midity structure of the lower troposphere. If there are no clouds, the marine boundary layer (MBL) is the classic mixed boundary layer. Humidity gradient and subsidence inversion are formed atop the mixed layer. When low clouds are present, long wave radia-tion and entrainment atop clouds form a strong temperature inversion and humidity gradient, which strengthen elevated ducts. How-ever, when Sc clouds are decoupled, a weaker temperature inversion and humidity gradient may occur between the surface mixed layer and subcloud layer, leading to a weak elevated duct atop the mixed layer.