Japan Geoscience Union Meeting 2023

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CG Complex & General

[A-CG30] Extratropical oceans and atmosphere

Sun. May 21, 2023 3:30 PM - 4:45 PM 201A (International Conference Hall, Makuhari Messe)

convener:Shion Sekizawa(Research Center for Advanced Science and Technology, University of Tokyo), Shota Katsura(Atmosphere and Ocean Research Institute, The University of Tokyo), Yuta Ando(Kyushu University), Shoichiro Kido(JAMSTEC Application Lab), Chairperson:Shion Sekizawa(Research Center for Advanced Science and Technology, University of Tokyo), Shoichiro Kido(JAMSTEC Application Lab)


4:15 PM - 4:30 PM

[ACG30-14] Diurnal cycle of precipitation over the Gulf Stream simulated by a regional atmospheric model

*Givo Alsepan1, Shoshiro Minobe1 (1.Hokkaido University)

Although the diurnal cycle of precipitation is not prominent over most mid-latitude oceans, recent studies show that an exceptionally strong diurnal cycle occurs over the Gulf Stream during summer. Diurnal peaks tend to occur in the early to late morning, with an oceanward phase propagation like what is commonly found in the tropics. A striking difference between the Gulf Stream and the tropical ocean is that strong amplitude enhancement is observed over the Gulf Stream, indicating the active role of the Gulf Stream in modulating the diurnal cycle. In this study, we conduct a numerical simulation for the first time on the diurnal cycle of precipitation over the Gulf Stream using the Weather Research Forecasting (WRF) model. We focus our simulation on July during which the diurnal cycle is most profound in the summertime. In general, the main features of the diurnal cycle are well simulated, including the oceanward phase propagations and strong diurnal amplitudes along the Gulf Stream with a clear gap in small amplitudes between the Gulf Stream and the continent. The reproducibility of the simulation indicates that the model can be used further for understanding the mechanisms of diurnal precipitation, especially to understand why oceanward phase propagation occurs over the Gulf Stream.