Answer:
rice
Explanation:
Answer:
The Earth is the third planet from the Sun.
Explanation:
The Earth is the third planet from the Sun, which is just the right distance for life to utilize the Sun's power and energy. Earth has two thirds of its surface covered by water and it is, up until now, the only planet to harbor life. It's atmosphere is rich in oxygen (which humans need to breath) and nitrogen. The sun's energy is crucial for Earth existence. Thanks to the atmosphere, the sun's energy reaches Earth attenuated. Otherwise, without atmosphere filtrating the sun rays and power, life as we know it wouldn't be possible.
Answer:
5
Explanation:
b. unable to tell from the information given
c. significantly less than 100 billion gallons
d. significantly more than 100 billion gallons
Answer:
b. unable to tell from the information given
Explanation:
We have only been given the amount of water rainforests receives in a year. No other information has been given. So also, we cannot make any further assumption and deduction from the information provided to us. In order to know the amount of water evaporated in a year, we should have been given the rate of evaporation in the rainforest. We cannot deduce the amount of water evaporated from this data.
Answer:
A
Explanation:
just took the test
10 km:
°C
50 km:
°C
80 km:
°C
Answer: 10 km is -50 degrees Celsius
50 km is 0 degrees Celsius
80 km is -85 degrees Celsius
Explanation:
Answer:
give me brin
Explanation:
The temperature of the atmosphere varies with altitude. Here are the approximate temperatures at each of the given altitudes:
1. 10 km:
At an altitude of 10 km, the approximate temperature is around -50 to -60 degrees Celsius. This altitude is within the troposphere, the lowest layer of the atmosphere, where temperature generally decreases with increasing altitude.
2. 50 km:
At an altitude of 50 km, the approximate temperature is around -70 to -80 degrees Celsius. This altitude is within the mesosphere, which is the third layer of the atmosphere. In the mesosphere, temperature decreases with increasing altitude, and it is colder compared to the troposphere.
3. 80 km:
At an altitude of 80 km, the approximate temperature is around -100 to -120 degrees Celsius. This altitude is within the thermosphere, the second highest layer of the atmosphere. The thermosphere is characterized by very low densities and high temperatures due to the absorption of high-energy solar radiation.
It is important to note that these temperatures are approximate and can vary depending on various factors such as time of day, season, and geographical location. Additionally, the temperature profiles can exhibit variations due to atmospheric phenomena such as inversions or anomalies.