![]() ![]() WAVE platform encourages your Online engagement with the Master Teachers. We provide you year-long structured coaching classes for CBSE and ICSE Board & JEE and NEET entrance exam preparation at affordable tuition fees, with an exclusive session for clearing doubts, ensuring that neither you nor the topics remain unattended. We have grown leaps and bounds to be the best Online Tuition Website in India with immensely talented Vedantu Master Teachers, from the most reputed institutions. Vedantu LIVE Online Master Classes is an incredibly personalized tutoring platform for you, while you are staying at your home. Such formation of clouds results in rainfall during the daytime. This kind of convergence results in the development and formation of clouds. It is observed that a low-level convergence of air is produced as the sea breeze and its surface flow gets terminated over land. This is supported by strong heating during the daytime and strong cooling is needed during nighttime. This takes place largely in absence of strong winds. In the coastal region, it is seen that sea breezes generally alternate with land breezes. ![]() Strong winds with a speed of more than 15km/h can subdue the effect of sea breeze. However, from the sea breeze definition, it can also be inferred that due to the presence of strong winds which flow offshore. The fair weather is often accompanied by drizzles. To describe sea breeze, we can say that these breezes are moderate. This is because during this time the temperature difference is maximum due to unequal heating from sun rays in the afternoon. Sea breeze mostly occurs in the spring and summer months. The temperature difference between landmass and waterbody results in a pressure difference due to the expansion of the air layer. The nature and strength of the sea breeze bear a direct relationship with the temperature difference between landmass and waterbody. As a result, now wind flows from the land towards the waterbody. ![]() At night, the pressure over the land is higher than the pressure over the waterbody. Land breeze is also called offshore breeze. As a result, soon after sunset the sea breeze dies away and the land breeze is formed. Landmass loses heat more quickly than waterbody. Sea breeze originates over the water body whereas land breeze occurs over the landmass. Sea breeze occurs during daytime and land breeze occurs during the night. The sea breeze and land breeze activity differ in origin, movement and time of formation. Usually, people who live within a 30-40km distance of the coast experience winds during the daytime with a speed of 10 to 20km per hour which are caused due to sea breeze. People who live near the coast can experience this gentle breeze. During spring and the months of summer is the time when does sea breeze occur mostly. This is how does sea breeze occur when the air starts flowing from the waterbody toward the landmass. Now air starts flowing from a region of higher pressure to a region of lower pressure. The air above the land now has lesser pressure compared to the air above the waterbody. As the air above the land expands it becomes less dense. Now as the air above the land gets heated up during the daytime, it starts expanding. The phenomenon involved in this heating is called convection. As a result, the air above the land gets heated up quickly during the daytime. Now since water absorbs heat better than landmass, water absorbs heat much more slowly than land. We all know that during the daytime the ocean and the land both get heated up. Since this breeze originates in water bodies, thus it is called sea breeze. The sea breeze definition says that sea breeze is a type of wind that flows from the inland of the ocean to the landmass. They vary information and also their direction of flow. Breezes of two types- sea breeze and land breeze. The temperature gradient of any type results in the formation of a breeze. Breeze is usually described as a moderate air current. To understand what is sea breeze, we first have to understand how breezes are formed. The difference between the sea breeze and the prevailing winds is that the sea breeze is more localized. Sea breeze usually moves from large bodies of water towards landmasses. Apart from the sea breeze, a land breeze is also observed. To describe sea breeze formation we have to focus on the pressure difference which is created by different heat capacities of water and lands that are dry. The sea breeze definition can be stated as the characteristic wind flow that takes place from sea to land, usually during the day. One can describe sea breeze as a wind system that is localized. ![]()
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