Answer:
D) As you drive faster in the rain more raindrops strike your windshield.
Explanation:
- The Doppler effect occurs when there is a change in the frequency of the source wave with respect to the motion of the observer.
- There is an apparent increase in the frequency of the emitted source when an observer moves towards the source.
- The wavelength stretches when an observer moves away from the emitting source.
- Consider the rain droplets fall towards the Earth in a slightly slanted towards eastwards. So, if you drive westwards, the frequency of the rain droplets hitting the windshield is higher.
- Similarly, if you drive eastwards, the frequency of the rain droplets striking your windshield will be lower.
5 ways to communicate better
Prepare yourself on the subject. ...
Structure your thoughts. ...
Keep it simple. ...
Listen to others with intent. ...
Engage well.
For an individual to succeed as well as for an organization to succeed, effective communication is crucial. Leaders who can articulate their ideas well are better at motivating and forming bonds with their staff. Furthermore, it's critical to positively and concisely convey your opinions.Whether or not communication is successful determines whether a relationship will succeed. Being able to explain your ideas clearly is only one aspect of effective communication; listening intently is another. It is the capacity to completely comprehend, to demonstrate empathy, and to provide feedback in light of the other person's answer. Simply said, it is the fruitful interchange of ideas and opinions between individuals or organizations.
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Not at all. Density on its own is not sufficient
It’s C for sure I took this awhile back but I still remember... so thermal equilibrium is when to object have the same temperature due to them touching and transferring temperature for example if we have two metal blocks and one them is hotter than the other when you put them together the heat transfers and makes them both the same temperature.
When saturated air is cooled, it simply reaches its dew point. Dew point is simply the temperature at which dew begins to form.
Dew point of saturated air is already pre-determined by how much water vapor the air contains. A state of saturation exists when the air is holding the maximum amount of water vapor possible at the existing temperature and pressure. The higher the dew point, the higher the moisture content of the air. Cooling does not change the dew point of saturated air, rather its the level of saturation.
So if the air has more moisture, dew will form at a higher temperature and vice versa, but dew point is NEVER EVER GREATER than the air temperature.