TY - JOUR
T1 - Self-consistent global transport of metallic ions with WACCM-X
AU - Wu, Jianfei
AU - Feng, Wuhu
AU - Liu, Han Li
AU - Xue, Xianghui
AU - Marsh, Daniel Robert
AU - Plane, John Maurice Campbell
N1 - Publisher Copyright:
© 2021 The Author(s).
PY - 2021/10/19
Y1 - 2021/10/19
N2 - The NCAR Whole Atmosphere Community Climate Model with thermosphere and ionosphere eXtension (WACCM-X) v2.1 has been extended to include the neutral and ion-molecule chemistry and dynamics of three metals (Mg, Na, and Fe), which are injected into the upper mesosphere-lower thermosphere by meteoric ablation. Here we focus on the self-consistent electrodynamical transport of metallic ions in both the E and F regions. The model with full ion transport significantly improves the simulation of global distribution and seasonal variations of Mg+, although the peak density is slightly lower (about 35ĝ€¯% lower in peak density) compared with the SCIAMACHY measurements. Near the magnetic equator, the diurnal variation in upward and downward transport of Mg+ is generally consistent with the "ionosphere fountain effect". The thermospheric distribution of Fe is shown to be closely coupled to the transport of Fe+. The effect of ion mass on ion transport is also examined: The lighter ions (Mg+ and Na+) are transported above 150ĝ€¯km more easily than the heavy Fe+. We also examine the impact of the transport of major molecular ions, NO+ and O2+, on the distribution of metallic ions.
AB - The NCAR Whole Atmosphere Community Climate Model with thermosphere and ionosphere eXtension (WACCM-X) v2.1 has been extended to include the neutral and ion-molecule chemistry and dynamics of three metals (Mg, Na, and Fe), which are injected into the upper mesosphere-lower thermosphere by meteoric ablation. Here we focus on the self-consistent electrodynamical transport of metallic ions in both the E and F regions. The model with full ion transport significantly improves the simulation of global distribution and seasonal variations of Mg+, although the peak density is slightly lower (about 35ĝ€¯% lower in peak density) compared with the SCIAMACHY measurements. Near the magnetic equator, the diurnal variation in upward and downward transport of Mg+ is generally consistent with the "ionosphere fountain effect". The thermospheric distribution of Fe is shown to be closely coupled to the transport of Fe+. The effect of ion mass on ion transport is also examined: The lighter ions (Mg+ and Na+) are transported above 150ĝ€¯km more easily than the heavy Fe+. We also examine the impact of the transport of major molecular ions, NO+ and O2+, on the distribution of metallic ions.
UR - https://www.scopus.com/pages/publications/85117596697
U2 - 10.5194/acp-21-15619-2021
DO - 10.5194/acp-21-15619-2021
M3 - Article
AN - SCOPUS:85117596697
SN - 1680-7316
VL - 21
SP - 15619
EP - 15630
JO - Atmospheric Chemistry and Physics
JF - Atmospheric Chemistry and Physics
IS - 20
ER -