Water anywhere in the world freezes into ice in the range of 28 - 32 degrees F. This is also true in Antarctica. The range depends on the amount of mineral in the water.
The atmospheric layer that has the greatest range of temperature is the troposphere. In the troposphere, water vapor plays a huge role in the fluctuation of temperatures.
The thermosphere is the layer of the atmosphere that has the greatest range in temperature, with temperatures increasing with altitude due to the absorption of solar radiation. Temperature in the thermosphere can vary from below -100°C at the bottom to over 2,500°C at higher altitudes.
The tundra biome typically has the greatest yearly temperature range, with very cold winters and short, cool summers. This wide range is due to its high latitude and lack of trees to moderate temperatures.
The Earth's temperature range can vary greatly depending on the location and time of year. On average, Earth's temperature ranges from about -50°C in Antarctica to about 50°C in hot desert regions.
There are no countries in Antarctica.
The main mountain range in Antarctica is the Transantarctic Mountain Range.
The temperature in Antarctica ranges from about -50°C to 0°C (-58°F to 32°F) during the summer months, and from about -60°C to -80°C (-76°F to -112°F) during the winter months. Antarctica is known for being the coldest place on Earth.
Mercury is a liquid over the greatest temperature range among the chemical elements, with a melting point of -38.83°C and a boiling point of 356.73°C.
In Antarctica, the average temperature in June can vary depending on the region. However, generally, temperatures can range from -15°C to -60°C during this month, making it one of the coldest months of the year in Antarctica.
in the US it is Fairbanks, Alaska. Average January temp is -9.7 F. Average July temperature is 62.4 F. Greatest seasonal temperature range on earth is in Siberia, where it ranges from 70 to -70 F. This is due to its continentality- it's landlocked.
The layer of the atmosphere with the greatest temperature range is the stratosphere. In this layer, temperatures increase with altitude due to the absorption of ultraviolet radiation by the ozone layer, leading to significant temperature variations. The temperature can vary from around -60°C (-76°F) at the lower stratosphere to about 0°C (32°F) near the stratopause, resulting in a substantial temperature range.