Data sets of the changes of the length of day (Delta LOD) measured by space
geodetic techniques and of the atmospheric angular momentum (AAM) derived
from global meteorological data by the National Meteorological Center (NMC)
and the National Centers for Environmental Prediction/National Center for
Atmospheric Research (NCEP/NCAR) are used to reanalyze and study the excita
tions of Delta LOD, and to examine and compare the contribution of each AAM
series to Delta LOD. The main results are as follows.
1. The AAM reanalyzed with the assimilated global meteorological data by NC
EP/NCAR are more accurate and have lower noise than the original AAM derive
d by NMC. The NCEP/NCAR-based AAM is more consistent with the changes of th
e length-of-day series.
2. The NCEP reanalysed AAM data may better explain the non-tidal LOD variat
ions on intraseasonal to interannual time scales, especially on the quasi-b
iennial time scale. The atmosphere cannot, however, explain all LOD variati
ons; other excitation sources are possible.
3. The effects of atmosphere on the estimated values of tides for Delta LOD
components up to a month are weak. The preliminary results of the annual a
nd semiannual tides can be estimated after removing the effects of atmosphe
re from Delta LOD.