To put it another way - the water molecules at the top surface of the sea (or pond, or puddle) are able to whizz off into the air (i.e. evaporate) (i.e. dry up) because they are moving fast enough to do so. The water further down does not escape because it is being squashed (held in) by the water at the top. Boiling point (100 degrees C) is the temperature at which the molecules in the water whizz about so fast that they are able to escape despite the weight of the water on top of them. If a puddle of rain water on the pavement is at normal temperature, the top layer will whizz away (dry up) continuously (slowly) until the whole puddle has dried up. If the water in a kettle is heated to 100 degrees C, it will be so hot that the water at the bottom will be able to escape (form bubbles) which are strong enough to resisit being squashed (kept in) by the water at the top.