The relationships between singular vectors (SVs) and transient features in
the background flow are examined through both composite techniques and case
-studies. The SVs are derived using the NOGAPS forward and adjoint tangent
models based on 48-hour forecasts during the NORPEX period. Composite resul
ts and case-studies both reveal significant spatial relationships between t
he SVs and transient features in the background flow. The SV perturbations
often occur below distinctive high potential-vorticity (PV) features in the
middle-to-upper troposphere. Case-studies reveal that the SVs propagate up
ward rapidly and have an impact on these PV features through the end of the
optimization interval. In order to investigate how these small, initial pe
rturbations have such a large impact on future development, the relationshi
p between SVs and the quasi-geostrophic forcing is examined through the use
of Q-vectors. The SV perturbations, while scaled to have a very small impa
ct on the temperature and wind fields, have a very large impact on the mid-
tropospheric Q-vectors. In contrast, the impact of the SV on the Q-vectors
is negligible when added to an analysis field for which it is not optimal (
e.g. the analysis field from another day). These findings establish a signi
ficant relationship between the SV perturbations and dynamically active reg
ions in the middle troposphere, and point toward an integral link between S
Vs and upper-level PV precursors in synoptic development.