Fig. 5: The relationship between 850-hPa air temperature, snowfall-to-total precipitation ratio, total precipitation, rainfall and the Arctic Oscillation.
From: Summer snow on Arctic sea ice modulated by the Arctic Oscillation
a–l, The June–August results for 1980–2020 of column 1 correlations with the Arctic Oscillation (AO), column 2 regressions onto the AO and column 3 linear response (composite difference) for 850-hPa air temperature (a–c), snowfall-to-total precipitation ratio (d–f), total precipitation (g–i) and rainfall (j–l), computed as the difference between the total precipitation minus snowfall. The yellow dots represent 95% statistical significance in a, d, g and j.
