Answer:
r = 0.7575
Explanation:
Result Details & Calculation
This is a strong positive correlation, which means that high X variable scores go with high Y variable scores (and vice versa).
X Values
∑ = 78
Mean = 15.6
∑(X - Mx)2 = SSx = 337.2
Y Values
∑ = 428
Mean = 85.6
∑(Y - My)2 = SSy = 57.2
X and Y Combined
N = 5
∑(X - Mx)(Y - My) = 105.2
R Calculation
r = ∑((X - My)(Y - Mx)) / √((SSx)(SSy))
r = 105.2 / √((337.2)(57.2)) = 0.7575
Meta Numerics (cross-check)
r = 0.7575
Üreme klonlama hakkında bilgi arayın ve
terapötik klonlama ve lehine iki ve argümana karşı iki argüman yazın.
KLON TİPİ
DONANIMDA
KARŞI
üreme
terapi
çevirisi budur.
This is a rhetorical strategy that strengthens the singer's argument.
<h3>What is rhetorical strategy?</h3>
- Words or phrases are used strategically to promote meaning.
- Word or phrases used to persuade readers.
- Words or phrases are used to further the author's goals.
By using a hypothetical example, Singer increases understanding of his argument. This is because it allows the audience to see the argument applied in a situation where anyone could be involved.
This makes the argument more understandable and can persuade the reader more easily.
For this reason, we can say that this example strengthens Singer's argument.
More information about rhetorical resources at the link:
brainly.com/question/25170004
The troposphere is the lowest layer of Earth's atmosphere, and is also where nearly all weather conditions take place. It contains approximately 75% of the atmosphere's massand 99% of the total mass of water vapor and aerosols.[2] The average height of the troposphere are 18 km (11 mi; 59,000 ft) in the tropics, 17 km (11 mi; 56,000 ft) in the middle latitudes, and 6 km (3.7 mi; 20,000 ft) in the polar regions in winter.
The lowest part of the troposphere, where friction with the Earth's surface influences air flow, is the planetary boundary layer. This layer is typically a few hundred meters to 2 km (1.2 mi; 6,600 ft) deep depending on the landform and time of day. Atop the troposphere is the tropopause, which is the border between the troposphere and stratosphere. The tropopause is an inversion layer, where the air temperature ceases to decrease with height and remains constant through its thickness.[3]
The word troposphere is derived from the Greek tropos (meaning "turn, turn toward, change") and sphere (as in the Earth), reflecting the fact that rotational turbulentmixing plays an important role in the troposphere's structure and behaviour. Most of the phenomena associated with day-to-day weather occur in the troposphere.
