Predictors of Zimbabwe summer rainfall are investigated with a view to improved long-range forecasts. Teleconnectivity is assessed in respect of sea-surface temperatures, the Southern Oscillation index, the Quasi-biennial Oscillation (QBO), outgoing longwave radiation (OLR) and wind. Spectral analys
Long-range predictability of Zimbabwe summer rainfall
✍ Scribed by L. S. Unganai; S. J. Mason
- Publisher
- John Wiley and Sons
- Year
- 2002
- Tongue
- English
- Weight
- 184 KB
- Volume
- 22
- Category
- Article
- ISSN
- 0899-8418
- DOI
- 10.1002/joc.786
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
The potential for long‐range prediction of Zimbabwe summer rainfall is investigated using an analysis of variance approach. It is assumed that the variance between seasons (inter‐annual variability) is made up of two components: the climate noise (intra‐seasonal variability) and signal (any variance above the noise). The magnitude of the climate noise is estimated by computing the variance of time‐averaged rainfall data based on a statistical model whose parameters are derived from observed daily values at each station. Results from the study indicate that up to approximately 70% of the total variance in Zimbabwe summer rainfall is potentially predictable at long range. Predictability is greatest during the last half of the rainy season, January to March, and much lower during October to December. The south section of the country shows relatively more predictability than the north. Comparisons between signal and noise are discussed in the context of long‐range predictability. The natural variability (noise) is proposed as a lower limit of the standard error of the estimate for any long‐range precipitation forecast for the country. Copyright © 2002 Royal Meteorological Society.
📜 SIMILAR VOLUMES
## Abstract Verma and Kamte (1980) and Joseph __et al.__ (1981) identified the association between Indian monsoon rainfall and 200‐mbar meridional wind index for the month of May, and indicated its potential for prediction of the seasonal rainfall. A detailed investigation has been made of this re
Hawaiian rainfall is teleconnected to short-term climate variability in the Pacific Ocean. The summer Southern Oscillation Index (SOI) and summer sea-level pressure (SLP) over the North Pacific are used as predictors, and the following winter rainfall indices from three islands of Hawaii are used as
## Abstract Hawaiian rainfall is teleconnected to short‐term climate variability in the Pacific Ocean. The summer Southern Oscillation Index (SOI) and summer sea‐level pressure (SLP) over the North Pacific are used as predictors, and the following winter rainfall indices from three islands of Hawai