Research Article

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

Figure 1

Ozone in CE (solid contour) and in SE (dashed contour) and difference of ozone between two experiments (SE−CE, shaded) at 70 hPa from May to September ((a–e), units: 10−7 mol/mol); (f–j) same as (a–e) but for zonal deviation of geopotential height (units: gpm, values in shaded area exceeding 80% confidence level). Difference of temperature zonal deviation between two experiments (SE−CE) at 70 hPa from May to September ((k–o), units: K).