converting geometric height to the corresponding geopotential height and calculating the h temperature and pressure at the corresponding geopotential height . In the height regime, the temperature (K) at geopotential height (km) is: T  288.15 6.5 for 0  11 (2a) T() −  216.65 for 11  20 (2b) T() 216.65 + (−20) for 20 32 (2c)   T() 228.65 + 2.8 (−32) for 32 47 (2d)   T()  270.65 for 47  51 (2e) T() 270.65 2.8 (−51) for 51 71 (2f)    T() – 214.65 2.0 (−71) for 71 84.852 (2g)    T() – and the pressure (hPa) at geopotential height (km) is: P  for 0   11 (3a) P()  for 11   20 (3b) P() for 20 32 (3c)    P() for 32 47 (3d)    P() for 47 51 (3e)    P() for 51 71 (3f) P()     for 71   84.852 (3g) P() In the second height regime, the temperature (K) at geometric height (km) is: T h 186.8673 for 86 91 (4a)   T(h) h for 91 100 (4b) T(h)   h  and the pressure (hPa) at geometric height (km) is: P h for 86 100 (5)    P(h) h where For reference, the temperature and pressure vs. geometric height are in Figs 1 and 2, respectively. FIGURE 1 Temperature vs. Geometric Height FIGURE 2 Pressure vs. Geometric Height
converting geometric height h to the corresponding geopotential height and calculating the temperature and pressure at the corresponding geopotential height . In the height regime, the temperature T (K) at geopotential height (km) is: T()  288.15 − 6.5 for 0  11 (2a) T()  216.65 for 11  20 (2b) T()  216.65 + (−20) for 20  32 (2c) T()  228.65 + 2.8 (−32) for 32  47 (2d) T()  270.65 for 47  51 (2e) T()  270.65 – 2.8 (−51) for 51   71 (2f) T()  214.65 – 2.0 (−71) for 71   84.852 (2g) and the pressure P (hPa) at geopotential height (km) is: P()  for 0   11 (3a) P()  for 11   20 (3b) P()  for 20   32 (3c) P()  for 32   47 (3d) P()  for 47   51 (3e) P()  for 51   71 (3f) P()  for 71   84.852 (3g) In the second height regime, the temperature T (K) at geometric height h (km) is: T(h)  186.8673 for 86  h 91 (4a) T(h)  for 91  h  100 (4b) and the pressure P (hPa) at geometric height h (km) is: P(h)  for 86  h  100 (5) where For reference, the temperature and pressure vs. geometric height are in Figs 1 and 2, respectively. FIGURE 1 Temperature vs. Geometric Height FIGURE 2 Pressure vs. Geometric Height
R-REC-P.835-6-201712-I!!MSW-E.docx