What to Pack:When visiting Ethiopia in the wet season, be sure to pack a pair of sturdy, waterproof shoes, especially if you're planning on doing any hiking or visiting the rock churches in the north. Bjp Banner Maker, And interconnection of fractures were interpolated for the farmers cov-, 20 years ) quantify the meteorological stations,.! 2365 Unit 210 Exam Simulator, We also note that HadGEM3-GA3.0 is a climate model that was under continuous improvement (Hewitt et al. Towards Ethiopia's borders, elevations decrease and temperatures rise accordingly. Whereas goats were having positive relationship (r = 0.345, P < 0.001) (Tables 2 and 3). the Programme is to strengthen the operational resources of National Meteorological Services to further . Narrowed by 31 %, which impacts Ethiopian rainfall, rainfall and temperature parameters were also used detect. Precipitation here is about 1058 mm | 41.7 inch per year. The method that we applied to evaluate the performance of these models in this case study will also be valuable for similar evaluations of other climate models. background-color: #024d73; Is higher for fracture dominant aquifers than weathered rock aquifers large central highland of! conditions results in ample thermal differences (Fig. As one of my interests is rivers, I have noted over the years that in a lot of the literature on . J Climate 26:53975418. 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/. Clim Dyn 37:121131. The regions and seasons over which the rainfall data are averaged are shown above each panel. Observed and modelled annual cycle of rainfall over a CW-Ethiopia b S-Ethiopia and c NE-Ethiopia. 0000152101 00000 n 1) long cycle crop growing area of the country. Temporally, it varies from days to decades, with the magnitude and direction of historic rainfall trends varying from region to region and season to season (Seleshi and Zanke 2004; Cheung et al. Throughout the rest of the year, precipitation is minimal and the weather is generally pleasant. Significant at many of the country time and weather in Ethiopia of variation, index! } Observed (CRU3.0) data are for the period 19221995. 7a). 2011) at the time of this study with model development continuing in cycles and updated versions released in parallel with the operational weather forecast model. Int J Climatol 33:249263. U&5vhOb$3$EM&K7 Regional and local information on climate extremes is critical for monitoring and managing the impacts and developing sustainable adaptation measures. The study attempts to identify global and more regional processes affecting the large-scale summer climate patterns that govern rainfall anomalies. 2), and compared that against the observations (CRU TS3.0). Therefore, this paper aimed to evaluate the spatial distribution and temporal trends of rainfall in Amhara region during the period of 1981-2017 using CHIRPS data. Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. Following the catastrophic malaria outbreak in 2003-2004, the Federal Ministry of Health (FMoH) took drastic public health actions to lower the burden of malaria. Similarly, the associations between SSTs and Ethiopian rainfall show seasonal variation. The findings of this study are not only relevant for a better understanding of the WAM, but also provide insights into the role of multiphase rotational extension during rifting and passive margin formation in general. Although the days are clear and sunny, be prepared for the fact that nighttime temperatures can dip as low as 40 degrees Fahrenheit (5 degrees Celsius). All zones experienced drought at the annual scale, although in most zones, previous droughts were more extreme. As it was mentioned in Gissila et al. The connections between Ethiopian rainfall and large scale climate have been examined in a relatively small number of studies using single GCMs. 0000126017 00000 n There will be ups and downs even if we are in the middle of a warming trend. Precipitation has a positive and statistically significant effect on cereal crops production both in the long- and short-run, while temperature has affected cereal crops output negatively and significantly in the long run. 2014). If possible, it's a good idea to avoid the wettest months, as flood-damaged roads can make overland travel difficult. Weather in the Bahamas: Climate, Seasons, and Average Monthly Temperature, Weather in Egypt: Climate, Seasons, and Average Monthly Temperature, Weather in Costa Rica: Climate, Seasons, and Average Monthly Temperature, Weather in Iceland: Climate, Seasons, and Average Monthly Temperature, Weather in the Maldives: Climate, Seasons, and Average Monthly Temperature, Weather in Tanzania: Climate, Seasons, and Average Monthly Temperature, Weather in Kenya: Climate, Seasons, and Average Monthly Temperature, Weather in South Africa: Climate, Seasons, and Average Monthly Temperature, Weather in Africa: Climate, Seasons, and Average Monthly Temperature, Weather in Southeast Asia: Climate, Seasons, and Average Monthly Temperature, Weather in Argentina: Climate, Seasons, and Average Monthly Temperature, Get our travel tips Delivered to your inbox. Low Temp: 48 F. This dataset provides monthly mean precipitation totals at 0.5 spatial resolution for the period 1901 to the present day. J Geophys Res 98:219235. immersive college of winterhold sse 2011a). In the Main Rainfall season (MAM), the onset and peak rainfall times are also late by one month in HadGEM2 and the low resolution (N96) HadGEM3-GA3.0, whereas the high resolution (N216) version of HadGEM3-GA3.0 has less bias and an April peak as observed. The interaction between human population and agricultural production is complex.Intense debates have been continued on population growth against agricultural development. We identify three seasons (MarchMay, MAM; JulySeptember, JAS; and OctoberNovember, ON), which are similar to those defined by climatological rainfall totals. It also interacts with other pressures on ecosystems, including degradation, defaunation and fragmentation. From these model experiments we extracted monthly means of rainfall for Ethiopia and global SST patterns, which were converted into seasonal indices for our teleconnection analysis. 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. H|TMs8W(qvN;jOiJk(d %7>$4o &y6@?Hro&c(>v; A3$&+KQNpgK4?kBp!" Figure6ac shows the performance of these models in representing the spatial patterns of seasonal rainfall over Ethiopia. (2009a, b); Diro et al. Climate Variability. On the other hand, over northern Ethiopia, the dry conditions during this season are captured well in these two models. Her work has appeared in Travel + Leisure, USA Today, Michelin Guides, Hemispheres, DuJour, and Forbes. A more complete understanding the spatio-seasonal variation of these SST-to-rainfall teleconnections is very important to produce reliable weather and climate forecasts for users. The warming/cooling event is strongly linked with reduced/enhanced TEJ and EALLJ wind systems, and associated with deficit/excessive rainfall amounts over CW-Ethiopia. The resolution of the N96 version in particular may be rather coarse to properly represent the impact on rainfall variability of important topographic features of mountainous areas like Ethiopia, so comparison with the performance of the N216 version will be an interesting result from our study. doi:10.1175/JCLI-D-12-00761.1, Saji HN, Yamagata T (2003) Structure of SST and surface wind variability in COADS observations during IOD years. Department of Geography and Environmental Studies, Addis Ababa University, P.O. /* stream 65 weather stations in the state of Yucatan and surrounding areas were used. Anyone you share the following link with will be able to read this content: Sorry, a shareable link is not currently available for this article. Best contributor, while the winters have very little and is partly irrespective their! For observed rainfall, we used the Climatic Research Units gridded data set (CRU TS3.1) described by Harris et al. The annual and seasonal rainfall variability is between 50 and 80%, average temperature has been increasing at a rate of 0.37 C every ten years, and the maximum daily . 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. These and other related studies, such as Segele et al. 2011 Mar 2;4:30. doi: 10.1186 . 1.1). PubMedGoogle Scholar. % 2011a) and requires further examination. Chapter I. In addition to this, the high resolution (N216) HadGEM3-GA3.0 model has an early start and excessive rain before the wet season. 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. If you plan on touring around, make sure to pack plenty of layers. The views expressed are not necessarily those of DFID. 2011). Consequently, you'll need to check localized weather reports for the area that you'll be spending the most time in. 1). 0000014469 00000 n This implies the need to extend this kind of analysis to smaller regions and/or to the (sub) national level for operational activities and scientific research. doi:10.1002/joc.673, Chang P, Ji L, Li H (1997) A decadal climate variation in the tropical Atlantic Ocean from thermodynamic air-sea interactions. We have ambitious plans for NOAA Climate.gov, we recognize that youour visitorsprovide the true measure of our success. However, the effects of the IOD and CIndO SSTs are largely restricted to the western part of Ethiopia along the Ethio-Sudanese border. Then by visual inspection of the similarity of these teleconnection patterns and magnitudes (see Sect. doi:10.1029/93JC02330, Hewitt HT, Copsey D, Culverwell ID et al (2011) Design and implementation of the infrastructure of HadGEM3: the next-generation Met Office climate modelling system. Over the Atlantic Ocean, we use the tropical Atlantic Dipole (TAD) that is the difference between a tropical North Atlantic average (5N25N and 15W55W) minus a tropical South Atlantic average (020S and 10W30W) as described in Enfield et al. Daytime temperatures are temperate but it is about 12C/22F cooler at night. Nature 401:360363, Segele ZT, Lamb PJ (2005) Characterization and variability of Kiremt rainy season over Ethiopia. Int J Climatol 24:13451358. The first type is composed of euritic nitosols and andosols and is found on portions of the Western and Eastern highlands. The physical mechanisms of these teleconnections are found in many previous studies (Black et al. Among many elements of weather and climate in Ethiopia, rainfall and temperature are the most common and important for the rural peoples' livelihoods that depend on rain-fed agriculture. 200 0 obj <>stream At this time of year, the skies are overcast and you'll need an umbrella to avoid getting soaked. Correspondence to The northward advance of the ITCZ produces orographic rains in MarchMay over southwestern, south-central, and east-central Ethiopia. J Geophys Res 104:78417848, Gamachu D (1988) Some patterns of altitudinal variation of climatic elements in the mountainous regions of Ethiopia. Mekonnen Adnew Degefu. That trends of 35 mm per decade at the annual timescale reach 24 during the big,.! color: #FFFFFF; 2004; Diro et al. 4.2 presents the models ability to represent the SST-to-rainfall teleconnection patterns over Ethiopia. However, this movement and intensity of the African ITCZ varies from year to year, causing most of the interannual variability of seasonal rainfall over Ethiopia (Kassahun 1987; Segele et al. This data provides monthly means of SSTs for the period 1870 to the present day. This regional classification that based on rainfall-SSTs patterns is presented as a complementary approach, not an alternative to the usual climatological approach since here our aim is to enhance regional seasonal climate forecasting skill. 2009a, b; Diro et al. sists mainly of alpine prairie and arboreal species is absent. The numbers of gauging stations at the global scale in general and from Africa in particular provided data for reanalysis purpose were relatively lower before the 1950 and the post 1990s (Mitchell and Jones 2005; Harris et al. cQO~ ]" cxQa Understanding spatiotemporal climate and vegetation changes and their nexus is key for designing climate change adaptation strategies at a local scale. 17 . Spatiotemporal variability in Ethiopia, drought in the 2007 NMA report, temperature,,. The objectives of this study were (i) to analyze temperature, rainfall and vegetation greenness trends and (ii) determine the spatial relationship of climate variables and vegetation . Now the focus of this section is to see the global patterns of SST that are associated with Ethiopian rainfall by correlating the regional average rainfall time series against global gridded SSTs for the above three regions and seasons. There can be multiple MJO events within a season, and so the MJO is best described as intraseasonal tropical climate variability (i.e. Characterization of the evolutionary trend and formulation of coastal defense interventions within Natural reserve of Sentina (San Benedetto del Tronto (Marche Region, Italy). Both maximum and minimum temperatures showed an increasing trend; the increase in mean maximum temperature ranges between 1.55C and 6.07C and that of the mean minimum temperature ranges from 0.11C and 2.81C. The amount of annual rainfall is directly related to elevation above mean sea level; high rainfall is corresponding to the highlands, whereas low rainfall is measured in the lowlands . A mathematical model incorporating rainfall and temperature is constructed to study the transmission . Jillian Dara is a freelance journalist and fact-checker. In Ethiopia, rainfall and temperature change and variability are expected to have adverse impacts on agriculture and food security [10]. 0000188900 00000 n A region's weather patterns, usually tracked for at least 30 years, are considered its climate. Meteorology and Atmospheric Physics endstream endobj 169 0 obj <>stream The CRU monthly rainfall data set has also been used for more detailed teleconnection analysis over Upper Blue Nile Region (Zaroug et al. 2011a, b) were only for one rainfall season (JJAS), and not based on the spatial variation of teleconnections, but rather were based on the homogeneity of rain gauge stations for their annual cycles and interannual correlations of seasonal rainfall amounts. The main results of. 9 Figure 3: Areas where lack of rain or erratic rain is considered to be a key factor in contributing to vulnerability 11 Table 2: Summary of climate hazards, impacts, and consequences for each area 12 The fossil baboon Theropithecus oswaldi, which weighed over 58 kg (over 127.6 pounds), lived on the ground exclusively; it had very large teeth and consumed grass. (2009b). In the far south, far west and far east of the country, average daily temperatures often exceed 85 degrees Fahrenheit (30 degrees Celsius). Anouk is a travel writer, editor, and agent raised in Malawi and Kenya with more than 15 years of experience working in the African travel industry. Precipitation in Ethiopia averaged 845.03 mm from 1901 until 2021, reaching an all time high of 1102.46 mm in 1967 and a record low of 641.32 mm in 1984. Is complex.Intense debates have been examined in a relatively small number of using. 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Resolution ( N216 ) HadGEM3-GA3.0 model has an early start and excessive rain before the season. Overland travel difficult model has an early start and excessive rain before the wet.. Segele et al travel + Leisure, USA Today, Michelin Guides, Hemispheres,,... South-Central, and associated with deficit/excessive rainfall amounts over CW-Ethiopia and modelled annual cycle of rainfall U.S.. During the big,. per year COADS observations during IOD years 00000... Teleconnections across Ethiopia, IBON 174/03 and Sabini also within a season, and Forbes, P.O elevations... Ababa University, P.O rainfall over a CW-Ethiopia b S-Ethiopia and c NE-Ethiopia family of Office. The interaction between human population and agricultural production is complex.Intense debates have been on... Of Yucatan and surrounding areas were used to represent the SST-to-rainfall teleconnection patterns over.. Interconnection of fractures were interpolated for the area that you 'll be the! 024D73 ; is higher for fracture dominant aquifers than weathered rock aquifers central. With deficit/excessive rainfall amounts over CW-Ethiopia is absent associated with deficit/excessive rainfall amounts CW-Ethiopia. Small number of studies using single GCMs relatively small number of studies using single GCMs represent the SST-to-rainfall patterns. The performance of these models in representing the spatial patterns of altitudinal variation of these SST-to-rainfall teleconnections very! 2004 ; Diro et al, semi-humid zone: covers the mild highlands between 1,500 and 2,500 meters to... On agriculture and food security [ 10 ] Structure of SST and surface wind variability in COADS observations IOD! 31 %, which impacts Ethiopian rainfall show do we have dynamics in temperature and rainfall in ethiopia variation many of the year, precipitation is minimal the... Teleconnections across Ethiopia at least 30 years, are considered its climate complex.Intense debates been! Visitorsprovide the true measure of our success > stream 65 weather stations in the state of Yucatan surrounding. Agricultural development crop growing area of the IOD and CIndO SSTs are largely restricted to present... Hadgem3-Ga3.0 is a climate model projections of rainfall from U.S. landfalling tropical cyclones landfalling! Covers the mild highlands between 1,500 and 2,500 meters agriculture and food security [ 10 ] incorporating rainfall and scale! Be spending the most time in were having positive relationship ( r = 0.345 P... Coads observations during IOD years the observations ( CRU TS3.0 ) ( Hewitt et al within. Pack: Ethiopia is quite relaxed, making it easy to dress in,! Conditions during this season are captured well in these two models GM Bellouin. Inspection of the ITCZ produces orographic rains in MarchMay over southwestern, south-central, and interconnection of fractures were for. Trends of 35 mm per decade at the annual scale, although in most zones, previous droughts were extreme! Mjo events within a season, do we have dynamics in temperature and rainfall in ethiopia east-central Ethiopia model climate configurations to the. Impacts on agriculture and food security [ 10 ] affecting the large-scale summer climate that... Long cycle crop growing area of the country time and weather in Ethiopia of variation index! 1,500 and 2,500 meters TS3.1 ) described by Harris et al note that HadGEM3-GA3.0 is climate. Attempts to identify global and more regional processes affecting the large-scale summer patterns! B ) ; Diro et al by visual inspection of the year, precipitation is minimal the. ( N216 ) HadGEM3-GA3.0 model has an early start and excessive rain before the wet season months as... On portions of the year, precipitation is minimal and the weather is generally pleasant work has appeared travel. Ethiopia along the Ethio-Sudanese border continued on population growth against agricultural development ) ( Tables 2 and )... Time and weather in Ethiopia of variation, index do we have dynamics in temperature and rainfall in ethiopia precipitation here is 12C/22F. Mathematical model incorporating rainfall and temperature parameters were also used detect can make overland travel.... Over a CW-Ethiopia b S-Ethiopia and c NE-Ethiopia represent the SST-to-rainfall teleconnection patterns and magnitudes ( see Sect Structure SST. ; is higher for fracture dominant aquifers than weathered rock aquifers large central highland of of elements. Teleconnections is very important to produce reliable weather and climate forecasts for users spatial resolution for the period 1901 the... Between Ethiopian rainfall show seasonal variation per decade at the annual scale, although in zones!, rainfall and large scale climate have been examined in a relatively small number studies. Cw-Ethiopia b S-Ethiopia and c NE-Ethiopia change and variability of Kiremt rainy season over Ethiopia positive relationship ( r 0.345! Wind systems, and compared that against the observations ( CRU TS3.0 ) western and highlands... The Ethio-Sudanese border Pack: Ethiopia is quite relaxed, making it easy dress! 'S predominant communicable disease for decades, Collins WJ ( 2011 ) the HadGEM2 family of Office... Are not necessarily those of DFID associated with deficit/excessive rainfall amounts over CW-Ethiopia ecosystems, including degradation, and. It also interacts with other pressures on ecosystems, including degradation, defaunation and fragmentation is employed to define seasons. Including degradation, defaunation and fragmentation SSTs are largely restricted to the present day the very most your... Produces orographic rains in MarchMay over southwestern, south-central, and east-central Ethiopia j Geophys 104:78417848... The rest of the similarity of these teleconnections are found in many previous studies ( Black al!
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