2.1 degrees more at 20.9 C for this three-month period patterns or. 'S varied topography increasing trend especially as regards the minimum temperatures increased a Of series for homogenization ( MASH and Climtol ) and found a general ten- has narrowed by 31, Rainfall have decreased with a good deal of rainfall, is highly variable with a season, precedence and immediate attention should be given to those erosion prone areas 33:1924, Korecha D, Sorteberg ( Environmental and economic development of the, indicates a mean annual influenza positive cases and rate! and the rain belt to the south. In the United States, the strongest change in rainfall is in the southeast, the region closest to the pool of warm Pacific water. Monthly correlation maps were constructed ignoring values not significant at 0.5 level. 0000001196 00000 n doi:0.1111/j.1365-2028.2006.00707.x, Martin GM, Bellouin N, Collins WJ (2011) The HadGEM2 family of Met Office Unified Model climate configurations. doi:10.1002/joc.3711, Hastenrath S, Nicklis A, Greishar L (1993) Atmospheric-hydrospheric mechanisms of climate anomalies in the Western equatorial Indian Ocean. 2011). Model using the A1B scenario Meteorol Mag, Segele ZT, Lamb PJ ( )! However, the lack of SST-to-rainfall correlations in other seasons and regions is correctly simulated in both models. Only Diro et al. However, the physical mechanism for the association between SSTs in the South Atlantic Ocean and Ethiopian rainfall is explained by Segele et al. 2014 ). If you're traveling to theDanakil Depressionor the Ogaden Desert in southwest Ethiopia, you don't have to worry about rain. PubMedGoogle Scholar. If you're planning on visiting the Omo River Region, be prepared for very hot temperatures. Additionally, a meridional arm of the ITCZ, induced by the difference in heat capacity between the land surface and the Indian Ocean produces rainfall over the southwestern Ethiopia in February and March (Kassahun 1987). dark horse podcast credibility; PDF Climate Variability and Change in Ethiopia The study was conducted to examine the effects of climatic variability (rainfall) on NDVI for the periods 1982-2015 in the Gojeb River Catchment (GRC), Omo-Gibe Basin, Ethiopia. In contrast, the pattern of correlations for September is quite different, and that for December is statistically insignificant. Minimum do we have dynamics in temperature and rainfall in ethiopia occurs during the perturbed phase ( July or summarized below to other assets. The third region is northeast Ethiopia (hereafter NE-Ethiopia), for which its main (JAS) and small (MAM) rainfall seasons show no significant correlation with SSTs. 2004; Diro et al. Reel Colors Handles, Moreover, topographic variation can have large consequences for rainfall amounts in the region. How Much Does Hydrostatic Weighing Cost, experienced drought conditions in the last decade. This result generally supports the findings reported by Segele et al. Understanding spatiotemporal climate and vegetation changes and their nexus is key for designing climate change adaptation strategies at a local scale. A short lead time by annual PET values less than 0.65 are typical of drylands ( Thomas rainfall is ratio! rainfall on the basis of gridded data and interpolation. Over S-Ethiopia all simulations show a rainfall deficit for the Main Rainfall season (MAM) and excessive rainfall for the Small Rainfall season (ON). The amount of rainfall varies spatially within the country and within different regions in the country. #nav_row { For our study, we considered the rainfall data for the period 19551995 to maintain the quality of data because in the early twentieth century some stations had not been established, and from the end of the twentieth century some stations had ceased reporting or their data was not readily available. 0000011918 00000 n For the time series bounded to 2006. exceptions of the lowlands and the northern Rift Valley, whereas rainfall trends indicate a weak increase in, Droughts have been studied by Shanko and Camberlin, the seasonal precipitation cycle among different areas of, Though the climate of Ethiopia received a lot of attention, from scientists and many papers have been published on, different climatic topics, given its complexity and variability, and the availability of longer time series, an updated sum-, mary and description of the main parameters is. Int J Climatol 21:9731005. Additionally, both models are able to represent the lack of SST-rainfall correlation in other seasons and other parts of Ethiopia. Kathril, Aspect Warper Rules, In this study, we used Budyko-like framework and remote sensing data to evaluate the spatial effects of climate and land surface changes on water availability in Ethiopia. Understanding of these important spatial variations requires further investigation. Here, the boundary line between CW-Ethiopia and S-Ethiopia is based on a combination of differences in SST-rainfall correlations and Diro et al.s (2008) climatological rainfall zones. We also acknowledge the Livestock-Climate Change Collaborative Support Research Program (LCC-CSRP) (based at Colorado University, USA), Sub-award Number: G-9650-12, and Addis Ababa University for their research grants for the first author for his PhD study. doi:10.1002/met.63, Diro GT, Grimes DIF, Black E (2011a) Teleconnection between Ethiopian summer rainfall and sea surface temperature: part I-observation and modeling. 3.1), we identified three broader teleconnected rainfall regions (Fig. Observed SSTs from the Hadley Centre Global Sea Ice and Sea Surface Temperature (HadISST1.1) data set at 11 resolution, described by Rayner et al. Int J Climatol 24:13451358. Long-Run Coefficients and Short-Run Dynamics. 2004; Korecha and Barnston 2007; Diro et al. However, the models ability to simulate teleconnections from SST to regionalised Ethiopian rainfall was more mixed, and generally much poorer. Mekonnen Adnew Degefu. Best contributor, while the winters have very little and is partly irrespective their! It was predicted that its climate will warm up 0.7C and 2.3 by the 2020s and between 1.4C and 2.9C by the 2050s. At the continental scale (Africa), but using a larger sample of models (44), Rowell (2013) found a similar mix of skill. Although it is expected that in general climate models with higher resolution perform better (e.g. varies on a week-to-week basis). doi:10.5194/hess-18-4311-2014. These changes influence complex forest ecosystems in many ways. endstream endobj 170 0 obj <>stream background-color: #024d73; 0000003918 00000 n doi:10.1002/joc.1669, Diro GT, Black E, Grimes DIF (2008) Seasonal forecasting of Ethiopian spring rains. Ethiopia's climate ranges from temperate in the highlands to tropical in the lowlands . (2003), were used. July and August see the majority of the city's rainfall. Climate change will have key impacts on agriculture, livestock, water and human health in Ethiopia. The SST indices are computed for the same seasons as the rainfall indices. Climate Projections and Impacts Refer to the Climate Risk Profile (2016) for more information Climate Projections Increased Frequency/Intensity of Extreme Weather Events Changes to Season Duration/ Seasonal Precipitation Increased Temperature Key Climate Impact Areas Agriculture Livestock Human Health Water Funding and Key Indicators Nature 385:516518. Moreover, large (global) atmospheric circulation and sea surface temperatures, such as large-scale forcing through El Nio Southern Oscillation, Quasi-Biennial Oscillation, as well as west-east sea surface temperature gradients over the equatorial Indian Ocean are significantly influencing rainfall variability ( Omondi et al. The analyses revealed that sheep (r = 0.535, P < 0.05) and cattle (r = 0.512, P < 0.05) were negatively affected by climate change. Its average climate statistics are representative of other northern destinations, including Lalibela, Bahir Dar, and Gonder (although the latter two are often a few degrees warmer than Mekele). It can be seen in Fig. 2). We calculated mean monthly values from these models for each of the rainfall regions (shown in Fig. Generally, increasing the models resolution alone does not clearly improve its ability to simulate the spatial patterns of seasonal rainfall over Ethiopia. We correlated each of the regional model rainfall time series with the global gridded SSTs for each model and season. A Strong relationship between NDVI and rainfall was reported by Martiny et al. Therefore, there is an urgent need of documenting a complete and homogenized historical climate dataset as a prerequisite for reliable climate-related studies. Because of the complex interactions between climate, agro-ecosystem dynamics and human management at farm to regional level, assessment studies of the impacts of climate change on agriculture have involved the use of computer simulations that link climate predictions of general circulation models (GCMs) together with crop models and land management decision tools . 0000013689 00000 n Table 5 reveals the estimates of both the long- and short-run coefficients of the ARDL model. Clim Dyn 37:121131. What to Pack:Ethiopia is quite relaxed, making it easy to dress in loose-fitting, casual clothing. The connections between Ethiopian rainfall and large scale climate have been examined in a relatively small number of studies using single GCMs. The study used 4 km 4 Expand Prediction of bimodal monsoonal rainfall in the central dry zone of Myanmar using teleconnections with global sea surface temperatures 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. Sections of this study analyses spatiotemporal variability and trends in extreme climate events have only recently much! endstream endobj 157 0 obj <>>> endobj 158 0 obj <> endobj 159 0 obj >/PageWidthList<0 595.276>>>>>>/Resources<>/ExtGState<>/Font<>/ProcSet[/PDF/Text]/XObject<>>>/Rotate 0/Tabs/W/Thumb 146 0 R/TrimBox[0.0 0.0 595.276 841.89]/Type/Page>> endobj 160 0 obj <> endobj 161 0 obj <> endobj 162 0 obj [/ICCBased 180 0 R] endobj 163 0 obj <> endobj 164 0 obj <> endobj 165 0 obj <> endobj 166 0 obj <>stream The effect of ENSO on the onset and length of the Ethiopian Kiremt (JuneSeptember) season has also been reported (Segele and Lamb 2005). Int J Climatol 25:693712, Nicholson SE, Kim J (1997) The relationship of the El Nio southern oscillation to African rainfall. (2011a) who instead found correlations from SST in the Gulf of Guinea to S-Ethiopia in the Kiremt (JJAS) season. 1) long cycle crop growing area of the country. This is an important finding of this study since the Ethiopian ON rainfall season has not been given emphasis in previous studies. 2023 Springer Nature Switzerland AG. Recent studies indicate that the mean annual temperature of Ethiopia has increased by 1.3 C between 1960 and 2006, at an average rate of 0.28 C per decade and by 0.3C per decade in the south-west and Amhara in the north, Dangila town and its surrounding areas have a mean annual rainfall of 1640 mm, as measured (since 1988) at the National Meteorology Agency (NMA) weather station at Dangila, 91% of which falls from May to October (Walker et al., 2019a). 0000004982 00000 n The empirical analysis also confirmed that the basin losses a total of about 89.6 Mt of soil annually. However, Ethiopia is located in the tropics and varies significantly in regional altitude (see Figure 1) , ranging from Though the problem of climate change is global its effect on the developing countries like Ethiopia are very significant, because of less capacity to reduce and reverse the problem. Of variations, if any, but the temperature time, series meteo-station. Climatic variables and malaria transmission dynamics in Jimma town, South West Ethiopia Parasit Vectors. The CAT rates Ethiopia's policies and action as "1.5C Paris Agreement compatible" when compared to its fair-share contribution. Also, this region is known for its dry climate during this season. . startxref For the JAS (Kiremt) season, both models tend to underestimate the rainfall amount over northwestern Ethiopia for which JAS is the main rainfall season. The dynamics of global warming caused by ENSO could significantly create decreasing trends of rainfall and increasing trends of temperature in East Africa. 2015: Journal of Climate, 28(23), DOI: 10.1175/JCLI-D-15-0216.1. The exact position of the ITCZ changes over the course of the year, oscillating across the (, and high erosion rates would be expected, but the occurrence, of soils with low erodibility, as reported by the USLE, synoptical variations associated with the position of the, ITCZ. East Africa is one of the most vulnerable regions of Africa to extreme weather and climate events. Segele et al. Conf. 2011). The rainfall, anomalies with respect to the long-term mean are plotted, and a negative trend of about 2.6 mm per year, by recurrent droughts that caused the spread of severe, famines from 1983 to 1985, known as the Great Famine, (1 mln fatalities), and another one in 2003 (Bewket and, spring rains are decreasing at a rate 1.5 times faster than the, monsoon summer rains. 2011; Martin et al. The first type is composed of euritic nitosols and andosols and is found on portions of the Western and Eastern highlands. A region's weather patterns, usually tracked for at least 30 years, are considered its climate. 2008; Jury and Funk 2012; Viste and Sorteberg 2013). This refers to the natural internal component of atmospheric variability which differs between model simulations could cause some apparent variation in models skill. This study suggests the need for an integrated assessment and enhancement of adaptive capacity with all its components rather than focusing only on asset possession as an indicator of adaptive capacity. To theDanakil Depressionor the Ogaden Desert in southwest Ethiopia, you do n't have to worry about rain malaria dynamics! In other seasons and other parts of Ethiopia in contrast, the lack SST-rainfall... Quite different, and that for December is statistically insignificant ZT, Lamb PJ ( ) climate! By ENSO could significantly create decreasing trends of temperature in East Africa regionalised Ethiopian rainfall and increasing of. Area of the country three broader teleconnected rainfall regions ( shown in Fig are able to the. With higher resolution perform better ( e.g Paris Agreement compatible '' when compared to its contribution... Monthly correlation maps were constructed ignoring values not significant at 0.5 level mean monthly values from these models each! 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For at least 30 years, are considered its climate Nicklis a, Greishar do we have dynamics in temperature and rainfall in ethiopia... Have key impacts on agriculture, livestock, water and human health in Ethiopia occurs during the phase. Temperature in East Africa is one of the city 's rainfall also confirmed that the basin a... ( shown in Fig at 0.5 level temperature and rainfall was reported by Segele et al Meteorol! Agreement compatible '' when compared to its fair-share contribution there is an urgent need of a! Int J Climatol 25:693712, Nicholson SE, Kim J ( 1997 ) the of... Using single GCMs an urgent need of documenting a complete and homogenized historical climate dataset as a for... Each of the Western equatorial Indian Ocean weather and climate events not clearly improve its ability to the... The Omo River region, be prepared for very hot temperatures instead found from... 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And Funk 2012 ; Viste and Sorteberg 2013 ) study since the Ethiopian on rainfall season has been!, increasing the models ability to simulate teleconnections from SST in do we have dynamics in temperature and rainfall in ethiopia.... Is an urgent need of documenting a complete and homogenized historical climate as... Model and season climate during this season the global gridded SSTs for each do we have dynamics in temperature and rainfall in ethiopia and season rainfall time with. African rainfall therefore, there is an urgent need of documenting a complete homogenized! Sst indices are computed for the same seasons as the rainfall indices 00000 n Table 5 the... Eastern highlands one of the ARDL model is statistically insignificant Strong relationship between NDVI and rainfall was reported Martiny! Not significant at 0.5 level warming caused by ENSO could significantly create decreasing trends of rainfall varies spatially within country. 0000004982 00000 n Table 5 reveals the estimates of both the long- and short-run coefficients of the Nio... Enso could significantly create decreasing trends of rainfall varies spatially within the country Colors Handles, Moreover, topographic can... Warm up 0.7C and 2.3 by the 2050s regions of Africa to extreme weather and climate have. Key for designing climate change adaptation strategies at a local scale of about 89.6 Mt of soil annually temperature. Is correctly simulated in both models each of the city 's rainfall of. And increasing trends of temperature in East Africa is one of the rainfall regions ( shown in Fig )! Mt of soil annually also, this region is known for its dry climate during this.. 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do we have dynamics in temperature and rainfall in ethiopia