Abox encloses the vertical line segments. horizontal line segments extend outward from both sides of the box to the plotted points at minus 1.2 and 3.3. all values are approximate. does this visual evidence support the results obtained in part b)? a. no because the boxplot supports that the lake is becoming more clear, since most differences are positive or near 0. b. yes because the boxplot supports that the lake is not becoming more clear, since most differences are positive or near 0. c. no because the boxplot supports that the lake is becoming more clear, since most differences are negative. d. yes because the boxplot supports that the lake is not becoming more clear, since most differences are negative.

"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:

47 - 90 = 43

43 - 180 = x

x = 137

c

step-by-step explanation:

there is vertical asymptote at x = 2 and x = 0

vertical asymptote occurs at the points where the denominator is 0. so we can say that

x = 2 occurs when there is a factor (x-2) in the denominator, and

x = 0 occurs when there is a factor "x" in the denominator

thus, the denominator of the equation would have "x * (x-2)", this is option c only. that's the correct answer.