yes
Cirrus clouds form at higher altitudes because they are composed of ice crystals that require cold temperatures to exist. These clouds typically form in the upper troposphere where temperatures are low enough for the ice crystals to form and remain suspended in the air.
Clouds form with ice crystals instead of liquid water droplets when the temperature is below freezing in the atmosphere. Ice crystals can also form in clouds that are very high up in the atmosphere where temperatures are colder.
Yes, the temperature of water affects how fast salt or sugar crystals dissolve. Higher temperatures typically result in faster dissolution because the water molecules move faster, increasing the rate at which they interact with and break down the crystal structures.
true/yes
they will burn out faster
Sugar crystals tend to grow faster than salt crystals because sugar molecules are larger and more prone to clustering together, allowing for quicker crystal formation. Additionally, sugar is more soluble in water compared to salt, which also contributes to faster crystal growth.
ones that are kept in high temperatures (the sun)
Particles move at a faster rate at higher temperatures, than they do at lower temperatures. This is do to the fact that heat is a form of energy. When a particle has more energy is moves faster.
Higher water temperature typically results in faster crystal growth because the molecules move more quickly, allowing them to collide and bond more rapidly. However, excessively high temperatures can also cause the crystals to dissolve or form incorrectly. It is important to find the optimal temperature range for crystal growth to achieve the desired results.
they are very high up in the atmosphere and since it is very cold up there ice crystals form instead of water droplets they then usually form a wispy looking cloud, sometimes they are called "mare's tails"
no can do
The high clouds (cirrus (Ci), cirrostratus (Cs), and cirrocumulus (Cc)) are composed of primarily nonspherical ice crystals with shapes ranging from solid and hollow columns to plates, bullet rosettes, and aggregates, with sizes spanning from about ten to thousands of micrometers. At cloud tops pristine small columns and plates are predominant, whereas at the lower part of the cloud bullet rosettes and aggregates are most common.