Scientific method and atomic structure add a co option 1: we will begin this topic by practicing the use of the scientific method. the steps of the scientific method are: observation, hypothesis, experiment results, and theory. using your understanding of the scientific method from your readings and lessons, you will be applying this knowledge to a real world situation. take a real world scenario in the news, or another outside source and apply the scientific method, being sure to detail the controls on your experiment. describe a result that would confirm your hypothesis • media option 2: choose a scientific paper written in the last year. the chamberlain library is a great source for this. for your chosen paper, look into the study and discuss how the scientific method was used in this paper. be sure to note they hypothesis, variables, results, etc. based on your understanding of the scientific method, be sure to discuss if you find this paper as a trustworthy top

What is the relationship between wind and ocean waves? question 17 options: wind moving at higher speeds will transfer more energy to the water, resulting in stronger waves. wind moving at higher speeds will transfer energy over a larger part of the ocean water, resulting in waves with a shorter wavelength. winds moving at higher speeds with cause water to move forward at faster rates, causing larger ocean waves. winds moving at higher speeds will affect deeper water, resulting in waves that move at a faster rate. how do temperature and salinity affect deepwater currents? question 15 options: as temperatures and salinity levels of water increase, the water rises to the surface where it creates currents as it moves to colder regions. they create changes in wind direction, moving denser water in the same direction as the wind and causing the deepwater circulation patterns found in the ocean. they equalize the forces on undersea currents caused by the coriolis effect as they replace more dense water with less dense water. they create density differences that cause dense deepwater currents to flow toward the equator where they displace less dense, warmer water above them.