It's really amazing how friendly, responsive and organized they are. They will always communicate with you every single time you send an email. The people whom you will interact with are super friendly - from the management company to the doorman to the person who will show you the apartment. However, this review is for whomever is interested:įirst of all, the process went by very smoothly. I was called for a viewing and later they asked me to sign off on documentation to send off to HPD, but I chose not to proceed. Wilks DS (2006) Statistical methods in the atmospheric sciences.So, I got called for one of these apartments. Whiteman CD (2000) Mountain meteorology, fundamentals and application. Simpson JE, Mansfiled DS, Milford JR (1977) Inland penetration of sea-breeze, fronts. NIMR (2014) Application of Boseong Global Standard Observatory (I), National Institute of Meteorological Research Miller STK, Keim BD, Talbot RW, Mao H (2003) Sea breeze: structure, forecasting and impacts. Lim HJ, Lee YH (2019) Characteristics of sea breezes at coastal area in Boseong. Lee YH, Ahn KD, Lee YH, Eom H (2020) Implementation of tidal parameterization in the weather research and forecasting (WRF) model. Lee YH, Ahn KD, Lee YH (2016) Parameterization of the tidal effect for use in the noah land-surface model: development and validation. Arch Meteorol Geophys Bioclim Ser A 34:3–26 Kessler RC, Eppel D, Pielke RA, McQueen J (1985) A numerical study of the effects of a large sandbar upon sea breeze development. Hersbach H et al (2020) The ERA5 global reanalysis. Boundary-Layer Meteorol 137:1–29įischereit J, Schlünzen KH, Gierisch AMU, Grawe D, Petrik R (2016) Modelling tidal influence on sea breezes with models of different complexity. Theor Appl Climatol 96:249–260Ĭrosman ET, Horel JD (2010) Sea and lake breezes: a review of numerical studies. QJR Meteorol Soc 115:547–570Īzorin-Molina C, Chen D (2009) A climatological study of the influence of synoptic scale flows on sea breeze evolution in the Bay of Alicante (Spain). For offshore flows, the tidal effect on wind-speed profiles is examined, with results showing that the tide state influences the time at which the sea-breeze speed increases but not the daily maximum speed of the sea breeze.Īrritt RW (1989) Numerical modeling of the offshore extent of sea breezes. This could be explained by the shorter distance to the sea due to the movement of the water boundary towards the station as well as larger sea–land temperature difference during high tide. The results indicate that there is a significant difference due to tidal state in the onset time of the sea breeze only for offshore flow, showing earlier arrival for the high-tide group in the morning than the low-tide group in the morning. The tidal effect on the sea breeze is tested at a significance level of 5% using a two-sample t-test for onshore and offshore flows. Sea-breeze days are divided into four groups depending on the tidal state and ambient flow direction. A sea-breeze day is defined as a day with both onset and cessation of a sea breeze within 24 h. We consider sea-breeze days during the warm season from May to September of each year from 2014 to 2017. The tidal effect on a sea breeze is examined using a 4-year 30-min database of wind-speed profiles obtained from a 300-m tower at a coastal site in Boseong, South Korea, facing a bay with tidal flats.

Sea breeze tower