Analysis of Rainfall Trends and Its Relationship with SST Signals in the Lake Tana Basin, Ethiopia

The impacts of climate change and climate variability on human life have led the scientific community to monitor the behavior of weather and climate variables at different spatial and temporal scales. This paper explores seasonal and annual trends of rainfall in the Lake Tana basin (LTB) and their t...

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Main Authors: Tesfay Mekonnen Weldegerima, Tadesse Terefe Zeleke, Belay Simane Birhanu, Benjamin Frederick Zaitchik, Zewdu Alamineh Fetene
Format: Article
Language:English
Published: Hindawi Limited 2018-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2018/5869010
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spelling doaj-3307d8b7e7e84bb2810cf2c32bea52cb2020-11-24T23:11:35ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172018-01-01201810.1155/2018/58690105869010Analysis of Rainfall Trends and Its Relationship with SST Signals in the Lake Tana Basin, EthiopiaTesfay Mekonnen Weldegerima0Tadesse Terefe Zeleke1Belay Simane Birhanu2Benjamin Frederick Zaitchik3Zewdu Alamineh Fetene4Atmospheric Physics, Bahir Dar University, P.O. Box 79, Bahir Dar, EthiopiaInstitute of Geophysics, Space Science and Astronomy (IGSSA), Addis Ababa University, Addis Ababa, EthiopiaCollege of Development Studies, Addis Ababa University, Addis Ababa, EthiopiaDepartment of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, MD 21218, USAAtmospheric Physics, Bahir Dar University, P.O. Box 79, Bahir Dar, EthiopiaThe impacts of climate change and climate variability on human life have led the scientific community to monitor the behavior of weather and climate variables at different spatial and temporal scales. This paper explores seasonal and annual trends of rainfall in the Lake Tana basin (LTB) and their teleconnections with global sea surface temperatures (SSTs) over the period between 1979 and 2015. The nonparametric Mann–Kendall test and Sen’s slope estimate are applied to the rainfall data collected from the National Meteorology Agency (NMA) of Ethiopia for detecting and estimating rainfall trends. Additionally, Pearson’s correlation coefficient method is used to determine the effect of SST variations on rainfall. The assessment of rainfall trends indicates that the amount of annual rainfall in the Lake Tana basin is increasing, but the rate of increase is not statistically significant. Seasonal analysis reveals that the smallest amount of rainfall occurs in the Bega season, and this season is getting drier with time. However, the analysis indicates that the other two seasons (Belg and Kiremt) are becoming wetter. The rainfall in Kiremt is increasing significantly (significant at the p=0.05 level) in Debre Tabor station with a rate of 10.20 mm/year. Besides, 78.1% of the total annual rainfall in the basin occurs during this rainy (Kiremt) season, whereas Bega and Belg contribute some 9.4% and 12.5%, respectively. Furthermore, the correlation analysis of rainfall and SSTs indicates that rainfall of the LTB is highly affected by the variations of SSTs.http://dx.doi.org/10.1155/2018/5869010
collection DOAJ
language English
format Article
sources DOAJ
author Tesfay Mekonnen Weldegerima
Tadesse Terefe Zeleke
Belay Simane Birhanu
Benjamin Frederick Zaitchik
Zewdu Alamineh Fetene
spellingShingle Tesfay Mekonnen Weldegerima
Tadesse Terefe Zeleke
Belay Simane Birhanu
Benjamin Frederick Zaitchik
Zewdu Alamineh Fetene
Analysis of Rainfall Trends and Its Relationship with SST Signals in the Lake Tana Basin, Ethiopia
Advances in Meteorology
author_facet Tesfay Mekonnen Weldegerima
Tadesse Terefe Zeleke
Belay Simane Birhanu
Benjamin Frederick Zaitchik
Zewdu Alamineh Fetene
author_sort Tesfay Mekonnen Weldegerima
title Analysis of Rainfall Trends and Its Relationship with SST Signals in the Lake Tana Basin, Ethiopia
title_short Analysis of Rainfall Trends and Its Relationship with SST Signals in the Lake Tana Basin, Ethiopia
title_full Analysis of Rainfall Trends and Its Relationship with SST Signals in the Lake Tana Basin, Ethiopia
title_fullStr Analysis of Rainfall Trends and Its Relationship with SST Signals in the Lake Tana Basin, Ethiopia
title_full_unstemmed Analysis of Rainfall Trends and Its Relationship with SST Signals in the Lake Tana Basin, Ethiopia
title_sort analysis of rainfall trends and its relationship with sst signals in the lake tana basin, ethiopia
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2018-01-01
description The impacts of climate change and climate variability on human life have led the scientific community to monitor the behavior of weather and climate variables at different spatial and temporal scales. This paper explores seasonal and annual trends of rainfall in the Lake Tana basin (LTB) and their teleconnections with global sea surface temperatures (SSTs) over the period between 1979 and 2015. The nonparametric Mann–Kendall test and Sen’s slope estimate are applied to the rainfall data collected from the National Meteorology Agency (NMA) of Ethiopia for detecting and estimating rainfall trends. Additionally, Pearson’s correlation coefficient method is used to determine the effect of SST variations on rainfall. The assessment of rainfall trends indicates that the amount of annual rainfall in the Lake Tana basin is increasing, but the rate of increase is not statistically significant. Seasonal analysis reveals that the smallest amount of rainfall occurs in the Bega season, and this season is getting drier with time. However, the analysis indicates that the other two seasons (Belg and Kiremt) are becoming wetter. The rainfall in Kiremt is increasing significantly (significant at the p=0.05 level) in Debre Tabor station with a rate of 10.20 mm/year. Besides, 78.1% of the total annual rainfall in the basin occurs during this rainy (Kiremt) season, whereas Bega and Belg contribute some 9.4% and 12.5%, respectively. Furthermore, the correlation analysis of rainfall and SSTs indicates that rainfall of the LTB is highly affected by the variations of SSTs.
url http://dx.doi.org/10.1155/2018/5869010
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