The eruption of Pinatubo blew thousands of tons of fine ash into the upper stratosphere. The ash clouds were carried all around the world, and increased the Earth's albedo, or reflectivity, enough so that enough sunlight was reflected back into space that the Earth actually began to cool down.
These eruptions have happened many times before; for example, the 1815 eruption of Mount Tambora in Indonesia caused the 1816 "Year Without A Summer", a time of widespread crop failures and famine.
The 1991 eruption of Mount Pinatubo released massive quantities of sulfur dioxide. This led to the formation of tiny droplets of sulfuric acid in the stratosphere. These reflected sunlight back into space, reducing global temperatures.
The temperature of the lava at Mount Pinatubo was estimated to be around 1,300 to 1,500 degrees Fahrenheit (700 to 800 degrees Celsius).
Global temperatures might cool by several degrees
Mount Vesuvius is an active volcano in Italy that reaches temperatures of around 1,000 degrees Celsius (1,832 degrees Fahrenheit) during eruptions. The surrounding area can experience temperatures well above 500 degrees Celsius (932 degrees Fahrenheit) during major eruptions.
The basalt lava from Kilauea volcano in Hawaii can reach temperatures between 1,070 to 1,170 degrees Celsius (1,958 to 2,138 degrees Fahrenheit). These temperatures can vary depending on the specific eruption and the type of lava being produced.
The 1991 eruption of Mount Pinatubo released massive quantities of sulfur dioxide. This led to the formation of tiny droplets of sulfuric acid in the stratosphere. These reflected sunlight back into space, reducing global temperatures.
The temperature of the lava at Mount Pinatubo was estimated to be around 1,300 to 1,500 degrees Fahrenheit (700 to 800 degrees Celsius).
Lava during a volcanic eruption can reach temperatures of 2000 degrees Celsius.
Global temperatures might cool by several degrees
Global temperatures might cool by several degrees
Mount Vesuvius is an active volcano in Italy that reaches temperatures of around 1,000 degrees Celsius (1,832 degrees Fahrenheit) during eruptions. The surrounding area can experience temperatures well above 500 degrees Celsius (932 degrees Fahrenheit) during major eruptions.
The basalt lava from Kilauea volcano in Hawaii can reach temperatures between 1,070 to 1,170 degrees Celsius (1,958 to 2,138 degrees Fahrenheit). These temperatures can vary depending on the specific eruption and the type of lava being produced.
In a hot and dry desert, temperatures may occasionally reach 50 degrees Celsius, or 122 degrees Fahrenheit . The norm in summer is 30 - 35 degrees C. Even in a hot desert, winter nights can be very cold, dropping to sub-zero temperatures Celsius.
Temperatures during volcanic eruptions can vary widely, ranging from 700 to 1,200 degrees Celsius (1,292 to 2,192 degrees Fahrenheit) for flowing lava, and even higher temperatures for pyroclastic flows and gas emissions. The exact temperature will depend on the type of volcanic eruption and the composition of the magma involved.
Mercury has a wide range of surface temperatures, with daytime temperatures reaching up to 800 degrees Fahrenheit (427 degrees Celsius) and dropping to -290 degrees Fahrenheit (-180 degrees Celsius) at night due to lack of atmosphere to retain heat.
In Summer, temperatures in the Gibson Desert can exceed 40 degrees Celsius. Maximum temperatures in Winter can be as low as 18 degrees C, whilst Winter minimums are quite cold, dropping to 6 degrees. Annual rainfall in the Gibson Desert is between 200mm and 250mm.
The sulfur cloud that comes out after a volcanic eruption covers the earth's atmosphere, stops much sunlight from reaching Earth, and makes the Earth colder by 2 to 3 degrees Celsius.