“…Being also season-dependent, sea breeze is augmented by high temperature difference between the sea and land. Most researchers report indeed on the higher amounts of dew that characterize the fall (and end of summer) season (Baier, 1966;Evenari et al, 1971;Goodman, 1985;Monteith, 1957;Rosenberg, 1974;Scherm & van Bruggen, 1993;Sharma, 1976;Tuller & Chilton, 1973;Zangvil, 1996;Zhang et al, 2015). Slow surface warming as a consequence of high heat capacity results on the other hand in high air pressure above the sea, leading to pressure gradient force, and subsequently to wind inflow (sea breeze) from sea to land (Miller, Keim, Talbot, & Mao, 2003).…”