Fig. 3: Fire weather conditions related to the East Asia jet stream.
From: Arctic wildfire carbon emissions strongly influenced by midsummer Tibetan Plateau precipitation
a‒d Linear regression of mid-summer jet stream northern edge (JSNE) index onto a vorticity (unit: 10−5 s−1), b total layer water vapor flux (vectors, unit: kg m−1 s−1) and its divergence (shading, unit: 10−5 kg m−2 s-1), c fire weather index (FWI), and d precipitation (unit: mm). The dotted areas are significant at the 95% confidence level.
