1. Temperature of water decrease due to their heat transfer to another medium. The media may be separated by a solid wall, so that they never mix, or they may be in direct contact. The heat exchanger changes the temperature of heat from hot to cold. It is meaning temperature of water is high when at inlet and heat exchanger reduce the temperature by transfer the heat to the low temperature at another fluid over a solid surface. So, the water comes out at outlet become low temperature.
The boiling point of sea water is higher compared with pure water. Temperature remain constant during boiling.
runoff from land
Rain water would normally boil at a slightly lower temperature than sea water, assuming the rain water has fewer dissolved particles in it compared to sea water.
Yes, sea water can freeze up to - 3 0C.
The sea often becomes calm at night due to a combination of factors, including reduced wind activity and changes in temperature. During the day, solar heating can create thermal winds, which stir up the water. At night, the cooling of the land and sea leads to a decrease in these winds, allowing the surface of the water to settle. Additionally, lower temperatures can stabilize the atmosphere, further contributing to calmer sea conditions.
Rising from the sea level to the higher levels will result in decrease of temperature and pressure.
Not directly you cant, but sea temperature does decrease with depth, although its not a straight line graph ( though depth : pressure is.)
Evaporation increase with the increase of temperature and decrease of pressure..
Water will boil at a lower temperature in a town located at 1000 m above sea level compared to sea level. On average, water boils at around 98.4 degrees Celsius at this elevation due to the decrease in atmospheric pressure.
No. A hypothesis would be "As the gradient of salt in the water increases the freezing point would decrease"
Gill movement begins to decrease in the sea by the fish.
The temperature of boiling water at sea level is 100 The temperature of boiling water at sea level is 211.149°F.
Water boils at a lower temperature as elevation increases due to the decrease in atmospheric pressure. On average, water will boil in a town located 1000 m above sea level at about 97.8 degrees Celsius (208 degrees Fahrenheit).
Sea level can fall due to factors such as the growth of glaciers on land, a decrease in the average global temperature, or a shift in ocean currents that redistributes water to lower latitudes. These changes can lead to less water being stored in the ocean and result in a drop in sea level.
Evaporation: Water evaporating from the surface will increase the salt concentration and hence the density of sea water. Dilution: An inflow of fresh water (rivers, rain) will dilute the salt solution leading to a decrease in density. Temperature: As the temperature of sea water increases it expands. As the volume increases, the density will decrease. Cooling will have the opposite effect. It should be noted that water has its highest density at 4 degrees C after which it starts to decrease. Pressure: Although it is considered that liquids cannot be compressed, some compression is in fact observed in deep oceans. The deeper you go, the higher the density of the sea water. Coriolis effect
The boiling point of sea water is higher compared with pure water. Temperature remain constant during boiling.
dead sea