1.] The boundary between two air masses of different density<span>. When it does not move, it's called "stationary"; "warm" when warmer </span>air<span> replaces cooler </span>air<span>; "cold" when cooler </span>air<span> replaces warmer </span>air<span>. Front: The transition zone </span>between two air masses<span> of... Cold front: </span><span>The boundary between two air masses.
2. </span><span>Continental polar (cP) or continental arctic (cA) </span>air masses<span> are cold, dry, and stable. ... Maritime tropical (mT) </span>air masses<span> are warm, moist, and </span>usually<span> unstable. Some maritime tropical </span>air masses<span> originate in the subtropical Pacific Ocean, where it is warm and </span>air<span> must </span>travel<span> a long distance over water.
3.] </span> <span>When a weather front passes over an area, it is marked by changes in temperature, wind speed and direction, atmospheric pressure, and often a change in the precipitation pattern...
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Answer:
m ≤ 60 (look at the picture)
Step-by-step explanation:
<em>5 greater than m is no more than 65</em>
m + 5 ≤ 65 <em>subtract 5 from both sides</em>
m + 5 - 5 ≤ 65 - 5
m ≤ 60
The answer to number 2 is $35, 200
Answer:
The function would be y = (1/3)x - 3
Step-by-step explanation:
The slope-intercept form is written in the form of y = mx + b where we leave "y" and "x" alone and plug in values for "m" and "b".
"m" is the rate of change while "b" is the initial value.
In this case, the rate of change given is 1/3. <em>Therefore, m = 1/3</em>.
The initial value given is -3. <em>Therefore, b = -3</em>
To figure out the function, all we have to do is plug in the values that we found for both m and b into the slope-intercept form:
y = mx + b
y = (1/3)x + (-3)
When we simplify this equation, we get:
y = (1/3)x - 3
