What is the advice?
Addation is a general term regarding the movement of fluids. This simply means transmission of material, energy or property, such as temperature or humidity by moving fluid - it can be liquid or gas. However, the term may have a number of more specific meanings depending on the context. It is most often used in the field of meteorology, where it usually refers to the movement of heat or humidity. In oceanography it is used to describe the transport of heat, dissolved substances - such as salt or suspended material by ocean currents. An example would be the transfer of heat at the distance of air streams. On the other hand, convection usually means mainly vertical movement of fluid in response to heating or surface cooling.
Addection can be positive or negative in terms of assets that are harassed. Where the direction of the wind is from higher to lower values for the property, it is considered to be positive because it increases the values of the wind. Converselyabout the wind. In connection with the temperature, the wind will blow from the warmer area to transport warm air, which increases the temperature, while the wind from the colder area will reduce the temperature. These scenarios can be called thermal counseling and cold counseling.
When predicting the weather, it is extremely important to take into account the advice. The map can be drawn to show, for example, a temperature distribution. Lines known as isotherm would combine points of the same temperature, and meteorologists can use the map to predict the probable temperatures for a given area from the relationship between isotherm and wind direction. Where the wind, often marked with arrows, exceeds isotherms, it can be expected that the temperature will rise or drop, depending on whether the wind flows from a warmer or cooler area. If the wind direction parallel to the isotherm, no temperature change would be expected.
moisture or moisture can also be transported by air movement and this is important when predicting the cloud cover, precipitation and fog. Where there is a currentEar from high humidity - for example from the warm ocean - can be expected to produce clouds and clotting. This is especially the case if the air is forced to rise to a colder level of local topography, which is a phenomenon known as orographic precipitation. A typical example would be the wind blowing from the ocean through a series of coastal mountains: humid air is forced to climb and cool as it rises, causing water vapor condensation into droplets, creating clouds that can lead to rain. When the greeting humid air cools down below the dew point of a cold surface, a joyful fog can be formed.