## ABSTRACT Agriculture in the state of Jharkhand depends on the southwest monsoon which brings about 80% of the mean annual precipitation. The high variability in rainfall generally leads to meteorological drought conditions, demanding a large time domain analysis of rainfall behaviour. In the pre
A note on the temporal and spatial variability of rainfall in the drought-prone Amhara region of Ethiopia
β Scribed by Woldeamlak Bewket; Declan Conway
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 211 KB
- Volume
- 27
- Category
- Article
- ISSN
- 0899-8418
- DOI
- 10.1002/joc.1481
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β¦ Synopsis
Abstract
The aim of this study is to characterise rainfall variability and trend in the droughtβprone Amhara Regional State of Ethiopia using standard rainfall statistical descriptors. A review of previous studies of Ethiopian rainfall shows different conclusions between studies about the existence of trends primarily due to their use of different periods of analysis. Various rainfall indicator series are presented and analysed for trend on annual, seasonal and daily time steps (including wetβday amounts and probabilities, percentiles and dry spell lengths). Two periods are used for analysis: 1975β2003 (12 stations) to optimise station density and 1961β2003 (five stations) to optimise record length in this relatively poorly monitored region.
A complex picture of rainfall variability emerges from the analysis, both in terms of spatial variability and temporal variability, from decadal to daily timescales. The results generally support those of the previous studies in Ethiopia with the additional findings that: (1) High levels of spatial variability exist at subregional scales in Ethiopia that are unlikely to be fully explained by largeβscale climate influences; (2) Choice of study period strongly influences the results of trend analysis in this region due to the effects of decadal variability (particularly because the 1980s was the driest decade and the 1990s the wettest decade on record); (3) Annual rainfall in the region recovered during the 1990s, although 2001β2003 were average or slightly lower; and (4) There are no consistent emergent patterns or trends in daily rainfall characteristics in this part of Ethiopia. Copyright Β© 2007 Royal Meteorological Society
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