A) Complete the table of values for y
b) Draw the graph of y = 2x + 3
on the grid.

Step-by-step explanation:

You should share the table that was given; your first job is to complete the table.  Setting up a table from scratch:

 x     y = 2x + 3      point (x, y)

 0     2(0) + 3 = 3    (0, 3)

 1       2(1) + 3 = 5     (1, 5)   and so on.

The y-intercept is (0, 3) (which is shown above), and the slope of the line is 2.  

Plot (0, 3).  Because the slope of the line is 2, we move 1 space to the right from (0, 3), to (1, 3) and then 2 spaces UP from (1, 3) to (1, 5).

Draw a straight line through (0, 3) and (1, 5).

"it's not the heat, it's the humidity".   that's a partly valid phrase you may have heard in the summer, but it's actually both.   the heat index, also known as the apparent temperature, is what the temperature feels like to the human body when relative humidity is combined with the air temperature.   this has important considerations for the human body's comfort.   when the body gets too hot, it begins to perspire or sweat to cool itself off.   if the perspiration is not able to evaporate, the body cannot regulate its temperature.   evaporation is a cooling process.   when perspiration is evaporated off the body, it effectively reduces the body's temperature.   when the atmospheric moisture content (i.e. relative humidity) is high, the rate of perspiration from the body decreases.   in other words, the human body feels warmer in humid conditions.   the opposite is true when the relative humidity decreases because the rate of perspiration increases.   the body actually feels cooler in arid conditions.   there is direct relationship between the air temperature and relative humidity and the heat index, meaning as the air temperature and relative humidity increase (decrease), the heat index increases (decreases).

step-by-step explanation:

alaska, florida, nevada, south dakota, texas, washington and wyoming, tenessee and new hampshire.

step-by-step explanation: