Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5

Figure 2

Vertical-latitude cross section of ozone ((a), units: 10⁻⁷ mol/mol), longwave heating rate ((b), units: 10⁻⁶ K/s), shortwave heating rate ((c), units: 10⁻⁶ K/s), and net radiative heating rate ((d), units: 10⁻⁶ K/s) difference between two experiments (SE−CE) along 56°E in June (shaded values from light to dark exceeding 90%, 95%, and 99% confidence level, resp.).

(a)

(b)

(c)

(d)