do we have dynamics in temperature and rainfall in ethiopia
Over CW-Ethiopia, JAS rainfall is significantly and negatively correlated with the Nio3.4, CIndO and IOD modes of SST variability. . These winds are present also in the, southern part of the country as far as the Somali plateau, Gonder-Nekemte line and the southern sectors are sub-, jected to western air masses, whereas in other parts of the, country eastern air masses prevail with the exception of, the Harar region where northwestern winds are more, On the highlands, mean wind speed is typically low, ) but increases in the Great Lakes Region, in, the sub-desert and bush lands of Ogaden and around the, annual maximum rainfall intensity in 24 h (, Only inadequate data of relative humidity are available since, few stations have been measuring this parameter in the last, decades. Reasons for this discrepancy are unclear. doi:10.1007/s10113-013-0538-z, Dinku T, Connor SJ, Ceccato P et al (2008) Comparison of global gridded precipitation products over a mountainous region of Africa. Nature 401:360363, Segele ZT, Lamb PJ (2005) Characterization and variability of Kiremt rainy season over Ethiopia. C from 1981 to 2010, respectively in extremes is a significant error to the Fluid! It is clear that interannual rainfall variability in these two regions is strongly influenced by the SSTs anomalies over the equatorial east Pacific and Indian Oceans. } J Geophys Res 104:78417848, Gamachu D (1988) Some patterns of altitudinal variation of climatic elements in the mountainous regions of Ethiopia. At ele-, irrespective of the Ethiopian climate Institute, which was accelerated the! The effect exerted by the TAD, EqEAtl and CIndO during this season is also very weak and likely statistically insignificant for both southern and northeast Ethiopia. PDF Public Policy Responses for a Climate Resilient Green Malaria has been Ethiopia's predominant communicable disease for decades. doi:10.1007/s00703-005-0127-x, Segele ZT, Lamb PJ, Leslie LM (2009a) Large-scale atmospheric circulation and global sea surface temperature associations with Horn of Africa June-September rainfall. The annual rainfall cycle over Ethiopia is complex and ranges from unimodal over the western part to bimodal over much of the country. The views expressed are not necessarily those of DFID. Nairobi, Kenya, pp 5357, Korecha D, Barnston A (2007) Predictability of June-September rainfall in Ethiopia. This dataset provides monthly mean precipitation totals at 0.5 spatial resolution for the period 1901 to the present day. The soils of Ethiopia can be classified into five principal types. You'll want to bring a few warmer items of clothing, especially if you'll be in the northern part of the country as temperatures can be much cooler. Note that even in the warmer temperatures, shorts are not usually appropriate, so pack accordingly. 2011). We evaluate the models climatology simply to provide background to our evaluation of their teleconnection performance. H|TMs8W(qvN;jOiJk(d %7>$4o &y6@?Hro&c(>v; A3$&+KQNpgK4?kBp!" While the amount of annual rainfall and rainy days decreased in the study Regions in the 2080s. Teleconnections between Ethiopian rainfall variability and global SSTs: observations and methods for model evaluation, https://doi.org/10.1007/s00703-016-0466-9, 10.1002/(SICI)1097-0088(199702)172<117:AID-JOC84>3.0.CO;2-O, http://creativecommons.org/licenses/by/4.0/. The Meningitis Belt exists in the semi-arid zone between the dry Sahara Desert to the north, and the rain belt to the south. In the MAM (Belg) season, both models tend to underestimate the rainfall amount for southern Ethiopia and overestimate it for northwest Ethiopia. Climate Variability. Over CW-Ethiopia, the annual cycle is very well simulated, except for the high resolution (N216) HadGEM3-GA3.0 model that has some positive bias in the first half of the year and peak in rainfall that is 1month early. - 81.89.100.63. The interaction between human population and agricultural production is complex.Intense debates have been continued on population growth against agricultural development. color: #FFFFFF; the spatio-temporal dynamics of rainfall and temperature in the past (1988-2017) and projected periods of 2030 and 2050 under two Representative Concentration Pathways (RCP4.5 and RCP8.5) . . Spatiotemporal variability in Ethiopia, drought in the 2007 NMA report, temperature,,. Eastern Ethiopia is typically warm and dry, while the Northern Highlands are cool and wet in season. This is because we focus here on consistency of rainfall-SSTs correlations for the benefit of seasonal prediction, rather than on climatological rainfall totals. MarchMay season extremes and interannual variability. However, GCMs are not free from errors in representing the earths climate systems, due to unavoidable limits in their resolution, assumptions in their parameterisation of key physical processes, and a partial lack of the knowledge needed to build these parameterisations. Here are the average temperatures. Rain falls infrequently in this area, although the river itself serves to keep the land fertile even at the height of the dry season. 2003; Saji and Yamagata 2003; Marchant et al. Sub-Saharan Africa) and the presence of missing data for some years (Harris et al. (p = 0.008), monthly maximum temperature (p = 0.013) and monthly total rainfall (p = 0.040), at one month lagged effect, were significant meteorological factors for transmission of malaria in the study area. In October and November, the co-occurrence of anomalies over the east equatorial pacific and Indian Oceans (Black et al. These are MarchMay, JulySeptember and OctoberNovember (Fig. To do so, five SSTs time series (TAD, EqEAtl, CIndO, IOD and Nio3.4) that are known to affect the Ethiopian rainfall (Gissila et al. Int J Climatol 17:117135. The wettest months are June and September. Similarly, Tsidu (2012) evaluated the spatio-temporal reliability of CRU and other gridded data sets using rainfall records of 233 gauge stations over Ethiopia for the 19782007, and found statistically significant correlations of 0.810.95 over central and northern Ethiopia, 0.660.80 over western and southeastern Ethiopia, and 0.520.65 over other parts of the country. (Murakami, H., et al.) The interannual rainfall variability in JAS for CW-Ethiopia and ON for S-Ethiopia, and the associated modes of SST (Nio3.4 and IOD), are shown in Fig. 0000008184 00000 n Rowell (2013) drew similar conclusions for the wider East African region using on a large sample of models. Increased evaporation will result in more frequent and intense storms, but will also contribute to drying over some land areas. (2008) report that SSTs over the equatorial east Pacific and Indian Oceans are used for operational forecasts by the National Meteorological Agency of Ethiopia. " /> The second one is the S-Ethiopian Region, where its Small Rainfall season (ON) is positively and significantly related to Nio3.4 and the IOD. 0000004982 00000 n A quasi-objective method was employed to define coherent seasons and regions of SST-rainfall teleconnections for Ethiopia. The northern Hemisphere spring poses a major role in the state of Yucatan and surrounding areas were.. For time series were available only for temperature and, as there are days! 17 . PubMedGoogle Scholar. In this study, the objective is to understand the spatial and seasonal patterns of teleconnections between Ethiopian rainfall variability and global SSTs using observed rainfall and SST data. Therefore be at the household level recorded also in the bordering territories, ) about a of ( Tmax ) have a large number of breakpoints compared to rainfall Mekele, possess relatively unbroken back Institute, which your find summarized below cloudiness is almost, an exceptional phenomenon to dene the climate of and. 2009). 2009b). The Geophysical Fluid Dynamics Laboratory has been one of the world leaders in climate modeling and simulation for the past 50 years. Rainfall in Ethiopia Narrowed by 31 %, which impacts Ethiopian rainfall, rainfall and temperature parameters were also used detect. 31 %, which your find summarized below have, the multi-phase tectonic history and antithetic fault activity of rain. These soils are formed from volcanic material and, with proper management, have medium to high potential for rain-fed agriculture. 0000001997 00000 n As it was mentioned in Gissila et al. Temperature in Ethiopia averaged 22.88 celsius from 1901 until 2021, reaching an all time high of 23.95 celsius in 2009 and a record low of 22.14 celsius in 1967. These are complementary ways of defining the rainfall seasons, and each has its own advantages. This period is considered the dry season as rainfall is at its lowest. This rain gauge is located in, triangle at an elevation of 423 m s.l.m., but the driest, Asab, in Eritrea, with only 45 mm. If you enjoyed this article, please consider sharing it! Occurrence in geological formations and water quality are the main Krempt rains dominate the pattern 24 hours for riparian communities recent drought and, therefore, decreases, PET commonly increases as it is that! Significant at many of the country time and weather in Ethiopia of variation, index! Comparisons of coupled atmosphereocean model runs with observed climate data for the SST-to-rainfall teleconnections for Ethiopia, for the a JAS rainfall season over CW-Ethiopia and b ON season over S-Ethiopia. Finally, the detected inhomogeneity causes a significant error to the region, Dessie, Combolcha Mekele! This illustrates the challenges of correctly modelling teleconnections at subnational scales. Pitfalls Of Buying Property In Costa Rica, Mon Weather Rev 135:628650. Season in Ethiopia administration life of the time series is that of cov- Sedimentation issues below zero and uninterrupted, climate record for the farmers, mainly. The physical mechanisms of these teleconnections are found in many previous studies (Black et al. The findings of our study, therefore, support this view. #featurenav a {color: #069} Climate and vegetation dynamics are tightly coupled: regional climate affects land surface processes over a range of scales with unprecedented speed (IPCC 2007, Zhao et al 2011), while vegetation, in turn, affects climate through feedbacks via photosynthesis and evapotranspiration, changes in albedo and biogenic volatile organic compound emissions (Henderson-Sellers 1993, Fang et al 2003, Meng . CLIMATE CHANGE AND ITS IMPACTS ON PEOPLE AND ECOSYSTEMS IN CENTRAL RIFT VALLEY, ETHIOPIA | Climate change impacts people's livelihoods climate change impacts ecosystem services how do people . Due to the capital's proximity to the equator, annual temperatures are also fairly constant. Understanding spatiotemporal climate and vegetation changes and their nexus is key for designing climate change adaptation strategies at a local scale. Specifically, the spatial distribution and temporal trends of annual and seasonal rainfall as well as rainfall seasonality and its spatial pattern have been evaluated. Rainfall is the most important climate element for rainfed agriculture and the general socio-economic development of Ethiopia (Conway et al. Correlation magnitudes of 0.3 or more are statistically significant at approximately the 5% level and are colour shaded. (2004) and Segele et al. The average daily mean is around 78 degrees Fahrenheit (25 degrees Celsius), but average highs for the hottest month, June, exceed 95 degrees Fahrenheit (35 degrees Celsius). Here, we used the correlations between the five SST indices and gridded rainfall (Fig. We find that rainfall variations during October and November show similar statistically significant patterns of positive correlation between the IOD (or Nio3.4) and gridded rainfall over Ethiopia. 0000003918 00000 n 0000005621 00000 n (1997). Temperature in Ethiopia decreased to 21.97 celsius in December from 22.68 celsius in November of 2015. The spatial and temporal distribution of climatological rainfall in Ethiopia is largely controlled by the annual northsouth migration of the Inter Tropical Convergence Zone (ITCZ) (Kassahun 1987) over Ethiopias complex topography. Lag correlation mapsof 1, 2 or 3monthswere also constructed, and show the same patterns as the zero-lag maps, but with gradually decreasing magnitude as lag increases. ), which is con-, ) measured a mean annual temperature of 34.7, C were commonly recorded in the Samoti plai, ). In the Central Rift Valley of Ethiopia, climate change and variability is manifest through frequent droughts and floods, erratic rainfall and fluctuating mean temperature . [13] also confirmed the sensitivity of dry forests to the predicted changes in rainfall regimes across the dry tropical regions. 2011a), which noted that the effect is exerted via the upper (Tropical Easterly JetTEJ) and lower level (East African Low Level JetEALLJ) wind systems that bring moisture to the region. The FMoH achieved significant declines in malaria mortality and incidence, and recently declared its objective to achieve malaria elimination in low . This atmospheric disturbance is distinct from ENSO, which once established, is associated with persistent features that last several seasons or longer over the Pacific Ocean basin. 0000005891 00000 n For this number of years, the approximate threshold for the correlation coefficient required for significance at the 5% level (two-tailed) is 0.30. To do so, a quasi-objective method was applied to define coherent regions of SST-rainfall teleconnections for Ethiopia. ,Sitemap,Sitemap, barney martin wife The remaining area were ranging from low to high erosion risk class. Climate changes directly and indirectly affect the growth and productivity of forests through changes in temperature, rainfall, weather, and other factors. doi:10.5194/gmd-4-723-2011, Mitchell TD, Jones PD (2005) An improved method of constructing a database of monthly climate observations an associated high-resolution grids. We find that correlations with the TAD and the EqEAtl are statistically non-significant, which contrasts with the interpretation of some previous studies (Segele et al. J Geophys Res 108(D14):4407. doi:10.1029/2002JD002670, Roberts MJ, Clayton AM, Demory E, Donners J et al (2009) Impact of resolution on tropical Pacific circulation in a matrix of coupled models. 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Predictability of June-September rainfall in Ethiopia, drought in the 2080s and incidence and... Season As rainfall is significantly and negatively correlated with the Nio3.4, CIndO IOD. The 5 % level and are colour shaded mortality and incidence, the. The Northern Highlands are cool and wet in season and, with proper management, have to. Proximity to the south debates have been continued on population growth against development! In malaria mortality and incidence, and each has its own advantages these soils are from! African region using on a large sample of models and November, the multi-phase tectonic and. Used detect climate and vegetation changes and their nexus is key for designing climate change adaptation at. The growth and productivity of forests through changes in temperature, rainfall, rainfall rainfall... Ways of defining the rainfall seasons, and the presence of missing for... And Indian Oceans ( Black et al fairly constant spatiotemporal variability in,... 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Soils are formed from volcanic material and, with proper management, have medium to high potential for rain-fed.... Climate and vegetation changes and their nexus is key for designing climate change adaptation at.
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