A study published in "Nature" estimates that during the last glacial maximum, low-to-mid latitude land surfaces at low elevation cooled on average by 5.8 °C relative to their present day temperatures. The study was based on an analysis of noble gases dissolved in groundwater rather than examinations of species abundances that have been used in the past.
A study published in Nature estimates that during the last glacial maximum low-to-mid latitude land surfaces at low elevation cooled on average by 5.8 ± 0.6 degrees C vs their present day temperatures. The study was based on an analysis of noble gases dissolved in groundwater rather than examinations of species abundances that have been used in the past.
A study published in Nature estimates that during the last glacial maximum, low-to-mid latitude land surfaces at low elevation cooled on average by 5.8 °C relative to their present day temperatures. The study was based on an analysis of noble gases dissolved in groundwater rather than examinations of species abundances that have been used in the past.
A study published in "Nature" estimates that during the last glacial maximum, low-to-mid latitude land surfaces at low elevation cooled on average by 5.8 °C relative to their present day temperatures. The study was based on an analysis of noble gases dissolved in groundwater rather than examinations of species abundances that have been used in the past.
