This will only take a few minutes. Pat the shrimp dry with a paper towel. Warm the oil or butter over medium-high heat: Tilt the pan as the oil warms, or butter melts, to coat the bottom of the pan. Add the shrimp to the hot pan: When the oil is hot and flows easily, add the shrimp to the pan. The shrimp should sizzle on contact (if not, warm your pan a little longer next time).
It is to be noted that the variations in salinity are the result of certain physical processes like evaporation, precipitation and freezing. Salinity decreases in case fresh water is added to the ocean water. It may be through any of the processes such as precipitation, influx of fresh water by rivers, surface runoff or the melting of snow and ice etc.
ocean surface temperatures are part of the forcing for the atmosphere, changes in high-latitude salinity distribution can be involved in climate change. In addition to its effect on seawater density, salinity is useful in itself as a tracer of ocean circulation and mixing. Salinity is established in the oceanâs surface layer by local processes, and therefore salinity variations within the ocean depend on the surface origin of a parcel of water. Mix-ing between waters of different salinities occurs within the ocean, and so the original salinity changes gradually. How-