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∙ 15y agoPatches of less hot goases in the photosphere are called sunspots.
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∙ 15y agoCooler regions in the Sun's atmosphere are known as sunspots. These areas appear darker than the surrounding regions because they are cooler, despite still being extremely hot compared to Earth. Sunspots are caused by magnetic activity on the Sun's surface.
Argon and trace gases like neon, helium, and methane make up less than 1 percent of Earth's atmosphere.
Yes, the Moon did have a very thin atmosphere called an exosphere. This exosphere is made up of very low-density gases, such as sodium and helium, that are constantly escaping into space due to the Moon's low gravity. The Moon's atmosphere is much less dense compared to Earth's atmosphere.
Hydrogen makes up about 0.000055% of Earth's atmosphere. It is much less abundant compared to other gases like nitrogen and oxygen.
The moon's gravity is too weak to hold on to an atmosphere. The lack of a magnetic field also causes the solar wind to strip away any gases that attempt to gather around the moon, resulting in the absence of a significant atmosphere.
The gases in the thermosphere include atomic oxygen, atomic nitrogen, and helium. This layer of the Earth's atmosphere has very low density, so the individual gas molecules are widely spaced apart.
Nitrogen rhen oxygen then argon and less than 1% of other gases
Argon and trace gases like neon, helium, and methane make up less than 1 percent of Earth's atmosphere.
As you move from the Earth's surface into outer space, the gases become less dense and the pressure decreases. The atmosphere becomes thinner, with the concentration of gases gradually decreasing as you travel higher. Eventually, once you reach outer space, the atmosphere becomes extremely thin, with almost no gases present.
CFCs (chlorofluorocarbons) currently make up less than 1% of greenhouse gases in the Earth's atmosphere.
The lighter coloured regions of the Moon are called highlands or less commonly as terrae.
Yes, the Moon did have a very thin atmosphere called an exosphere. This exosphere is made up of very low-density gases, such as sodium and helium, that are constantly escaping into space due to the Moon's low gravity. The Moon's atmosphere is much less dense compared to Earth's atmosphere.
The rare gases, also known as noble gases, make up about 1% of the Earth's atmosphere. This includes gases like helium, neon, argon, krypton, xenon, and radon. These gases are considered rare because they are present in very small concentrations compared to other gases like nitrogen and oxygen.
As you travel higher in Earth's atmosphere, the composition of gases changes in terms of their concentration. Oxygen, nitrogen, and argon are the most abundant gases in the lower atmosphere, while the percentage of oxygen decreases and other gases like helium and hydrogen become more prevalent in the upper atmosphere. The overall pressure also decreases with altitude, causing the air to become less dense.
The layered gases in the atmosphere are separated by their density and composition. As you move higher into the atmosphere, the gases become less dense and more homogeneous in composition. The layers are primarily defined by temperature variations, with distinct boundaries such as the tropopause and stratopause.
Eris has a very thin atmosphere that is primarily composed of nitrogen and methane gases. Its atmosphere is estimated to be only about 0.12 to 0.2 microbars in pressure, which is significantly less dense than Earth's atmosphere.
The atmosphere is primarily composed ofNitrogen (N2), which accounts for 78%.Oxygen follows, accounting for 20% of its volume, withArgon less than 1%.
Hydrogen makes up about 0.000055% of Earth's atmosphere. It is much less abundant compared to other gases like nitrogen and oxygen.