Skip to main content
. Author manuscript; available in PMC: 2021 Mar 23.
Published in final edited form as: Atmos Chem Phys. 2020 Mar 23;20(6):3373–3396. doi: 10.5194/acp-20-3373-2020

Table 4.

Statistical analysis of modeled RH using ozonesonde and aircraft observations.

N Mean R NMB NME
Observation Model
 Ozonesonde

 US and Canada

 – boundary layer 1016 57.70 67.07 0.73*** 16.2% 24.5%
 – free troposphere 881 39.16 43.31 0.83*** 10.8% 29.7%
 – upper model layer 398 7.81 8.72 0.79*** 11.6% 62.3%

 Asia

 – boundary layer 283 65.89 79.63 0.45*** 20.8% 28.7%
 – free troposphere 184 46.26 51.52 0.38*** 11.4% 47.7%
 – upper model layer 43 18.96 26.47 0.63*** 39.6% 67.2%

 Europe

 – boundary layer 1485 63.84 68.92 0.73*** 8.0% 17.1%
 – free troposphere 1368 36.14 42.82 0.80*** 18.5% 32.6%
 – upper model layer 679 7.13 9.56 0.91*** 34.1% 56.1%

 Aircraft

 – troposphere 126 41.66 52.04 0.84*** 24.9% 28.7%

Note: significance levels by Student’s t test for correlation coefficients between observations and simulations are marked as

*

p<0.05,

**

p<0.01, and

***

p<0.001, and lack of a mark indicates no significance. The 5h averaged hourly modeled relative humidity is used for ozonesonde data. The 2–4h averaged hourly modeled relative humidity is used for aircraft data to fully cover each observation time, and original aircraft data are averaged into 100m resolution to be compared with the model.