q 2003 American Meteorological Society Sampling Errors in Rawinsonde-Array Budgets

Rawinsonde data used for sounding-array budget computations have random errors, both instrumental errors and errors of representativeness (here called sampling errors). The latter are associated with the fact that ra-diosondes do not measure large-scale mean winds and state variables, but are contaminated by small-scale variations as well. Data from the western Pacific and the summer monsoon of southeast Asia are used to estimate these random errors, and to propagate them through budget computations to assign error bars to derived quantities. The statistics of sampling errors in directly measured variables are estimated from station pair analysis, in which variance is partitioned into contributions by resolved and unresolved scales. Resolved scales contribute the portion that is contained in averages of adjacent sounding stations and/or adjacent launch times (6-h intervals), while the rest of the total variance is defined as unresolved. Magnitudes of unresolved variability for typical rawinsonde-array spacings are;0.5 K for temperature;;5 % for relative humidity at low levels, rising to nearly 15 % in the middle-upper troposphere; and;2 m s21 for winds, rising to 3 m s21 in the upper troposphere. These are much larger than random instrumental errors, as estimated from pairs of simultaneous rawinsondes launched very close together. Vertical correlation scales of unresolved variability are 100–200 hPa. Up to 50% of the variance of humidity is unresolved, while for zonal wind the unresolved portion is only a few percent