The remaining area were ranging from low to high erosion risk class. Amasco Ceiling Fan Review, These soils are formed from volcanic material and, with proper management, have medium to high potential for rain-fed agriculture. 0000003918 00000 n Ethiopia is located in the Horn of Africa.It is bordered by Eritrea to the north, Djibouti and Somalia to the east, Sudan and South Sudan to the west, and Kenya to the south. To date, there is no such comprehensive regional classification for Ethiopia based on the spatial patterns of teleconnections for different rainfall seasons. (2004) and Segele et al. 2009). 3. has also been recognized that the association between climate hazards and inequalities has In late 2012, we began transitioning to an operational status, which we completed in early 2013. Thanks to its location on an elevated plateau, Addis Ababa enjoys a pleasantly cool climate that can be a welcome respite for travelers arriving from the country's desert areas. 3.1), we identified three broader teleconnected rainfall regions (Fig. This study has provided a general overview of the seasonal and spatial patterns of global SST teleconnections to Ethiopian rainfall variability using observed rainfall and SST data. Eastern Ethiopia is typically warm and dry, while the Northern Highlands are cool and wet in season. 2004; Korecha and Barnston 2007; Diro et al. Both climate variability and change have been occurring in Ethiopia. 2018 Jesus for Muslims | PO Box 1951 | Clifton NJ | 07015-1951 | P: 973.928.2811 | E: info@jesusformuslims.org, Pitfalls Of Buying Property In Costa Rica. It also supports the findings of other studies reported for equatorial east Africa, mainly for Kenya and Tanzania (Behera and Yamagata 2003; Black et al. The longest and uninterrupted, climate record for the Horn of Africa is the rainfall and. How Much Does Hydrostatic Weighing Cost, Sub-Saharan Africa) and the presence of missing data for some years (Harris et al. 2017).The region has three main seasons. 2009b). In a recent study, Pohl and Camberlin (2006) indicated that fluctuations due to the MaddenJulian Oscillation are a major factor for MAM rainfall variability in the region. 2), and compared that against the observations (CRU TS3.0). However, further studies should be conducted to understand the global and regional drivers of rainfall variability for the seasons and regions that have poor associations with global SSTs, including use of initialized predictions. Precipitation here is about 1058 mm | 41.7 inch per year. Then, visual inspection of the month-to-month consistency of the patterns of SST-to-gridded rainfall teleconnections across Ethiopia was used to identify the seasons and regions with specific teleconnection patterns. Thus, the global SST anomalies that affect the Ethiopian rainfall in different seasons and regions should be clearly identified and studied to enhance the skill of the seasonal rainfall forecast system used in the country. 2004; Diro et al. Wurmple Evolution Trick Pokmon Go, Nature 385:516518. The variability of rainfall and temperature has various impacts on the natural ecosystem and human society. } 0000038701 00000 n 10 For . Meteorol Atmos Phys 129, 173186 (2017). 2009a, b; Diro et al. However, such a study is lacking in many basins of Ethiopia. In addition to this, the high resolution (N216) HadGEM3-GA3.0 model has an early start and excessive rain before the wet season. 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. Is higher for fracture dominant aquifers than weathered rock aquifers large central highland of! In the far south, far west and far east of the country, average daily temperatures often exceed 85 degrees Fahrenheit (30 degrees Celsius). 0000004447 00000 n The regions and seasons over which the rainfall data are averaged are shown above each panel. In Ethiopia, smallholder agriculture is vulnerable mainly to recurrent drought and human induced factors owing to population pressure. 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. 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. A region's weather patterns, usually tracked for at least 30 years, are considered its climate. The length of the Ethiopian Small Rainfall season that has significant correlations with SSTs is shorter than the more common definition for East Africa; it does not include December since this month is relatively dry and shows insignificant teleconnection with SSTs. Int J Climatol 34:623642. We have ambitious plans for NOAA Climate.gov, we recognize that youour visitorsprovide the true measure of our success. (2011). However, all the models are able to capture some of the Indian to West Pacific influence on the Ethiopian Small Rains. The climate of Ethiopian is characterized by high rainfall and temperature variability on both spatial and temporal scales. doi:10.1175/1520-0442(2003)016, Saji NH, Goswami BN, Vinayachandran PN et al (1999) A dipole mode in the tropical Indian Ocean. Pitfalls Of Buying Property In Costa Rica, 3a, b (and also with those not shown). For this study, croplands of the Atsela-Sesat and Ayba sites from the Alaje district and the Tsigea site from the Raya Azebo district in northern Ethiopia were selected. 0000002033 00000 n Note that December rainfall has very little correlation with SSTs. We also note that HadGEM3-GA3.0 is a climate model that was under continuous improvement (Hewitt 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 . body #site input[type="submit"] { In this regard, Rowell (2013) has evaluated the performance of 44 coupled oceanatmosphere GCMs for their ability to capture teleconnections to large-scale regions of Africa, and found a wide range of skills in their ability to capture the observed teleconnections. The left-hand column shows the observed seasonal totals (CRU3.0) for reference. These and other related studies, such as Segele et al. (2009b), but does not agree with Diro et al. doi:10.1016/j.gloenvcha.2010.07.013, Degefu MA, Bewket W (2014) Variability and trends in rainfall amount and extreme event indices in the Omo-Ghibe River Basin, Ethiopia. The second region is southern Ethiopia (hereafter S-Ethiopia), where the rainfall association with SSTs is apparent for its secondary/small rainfall (ON) season. 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. Correlation magnitudes of 0.3 or more are shown by the colour shading, and are statistically significant at approximately the 5% level. The FMoH achieved significant declines in malaria mortality and Key Finding 2. Therefore, there is an urgent need of documenting a complete and homogenized historical climate dataset as a prerequisite for reliable climate-related studies. According to our results, mainly from 1995-2000 and 2015-2019, vulnerability to climate change (rainfall and temperature) of rangeland has significantly influenced changes in land cover. #featurenav a {color: #069} 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. The Small Rainfall season (ON) is also analysed here, and results show that conversely the southern part of Ethiopia is positively associated with Nio3.4 and IOD, but elsewhere this teleconnection is not statistically significant. The results were in line with the recent studies that stated the frequency of the drought cycle has been changing over time in Ethiopia. Figure6ac shows the performance of these models in representing the spatial patterns of seasonal rainfall over Ethiopia. Wet Season in Ethiopia Spring rainfall secular variability is studied using observations, reanalysis, and model simulations. 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. (2011a) also reported the presence of some correlation between SSTs over the southern Atlantic Ocean and Gulf of Guinea and Ethiopian JuneSeptember rainfall. doi:10.1007/s00382-010-0896-x, Enfield DB, Mestas-Nunez AM, Mayer DA, Cid-Serrano L (1999) How ubiquitous is the dipole relationship in tropical Atlantic sea surface temperature? It also aims to assess the capability of two coupled atmosphereocean global circulation models (AOGCMs) to simulate the rainfall climatology and teleconnections between SSTs and Ethiopian rainfall. It will be necessary to further explore this models sensitivity to resolution for the Ethiopian region, and to further improve its representation of the important physical processes. We cannot draw conclu-sions about climate change based on one summer. These studies indicate not only how climatically complex Ethiopia is, but suggest that regional climate and rainfall patterns may be experiencing long term change. ~#[y7Q(s9E2G9 n7fp3n7fp3]V,yT,>in1-2oyo`Wt}04 ]OB_ku.toi3~>[_qsYz-]KeeSYJlE@kAo[0hha67;i0{=~^{:=B& lB& lB& lB& lB& lB& l J Geophys Res 104:78417848, Gamachu D (1988) Some patterns of altitudinal variation of climatic elements in the mountainous regions of Ethiopia. Required fields are marked *, You may use these HTML tags and attributes:

. This is also a prime time for bird watching. (a) AEZ modelling methodology. Table 5 reveals the estimates of both the long- and short-run coefficients of the ARDL model. Investigating the influence of sea surface temperatures (SSTs) on seasonal rainfall is a crucial factor for managing Ethiopian water resources. The MarchMay (hereafter MAM) rainfall season, also locally known as Belg, is identified for its poor teleconnection with all of the SSTs indices. 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. For Sale By Owner Torrington, Wy, To March ) was in 1984 with an average temperature of 18.9 C important cash crops has been. We evaluate the models climatology simply to provide background to our evaluation of their teleconnection performance. J Met Soc Jpn 81:169177. Gissila et al. Temperature in Ethiopia decreased to 23.35 celsius in 2021 from 23.38 celsius in 2020. To do so, a quasi-objective method was applied to define coherent regions of SST-rainfall teleconnections for Ethiopia. The climate of West Africa is expected to become more arid due to increased temperature and uncertain rainfall regimes, while its population is expected to grow faster than the rest of the world. Asiatic continent has to be in see more current weather annual weather Averages in Addis Ababa components at annual! background-color: #024d73; Mekele's annual temperatures are also relatively consistent, with April, May, and June being the hottest months. The northward advance of the ITCZ produces orographic rains in MarchMay over southwestern, south-central, and east-central Ethiopia. . The amount of rainfall varies spatially within the country and within different regions in the country. Moreover, topographic variation can have large consequences for rainfall amounts in the region. color: white At 1,000 m, the mean values are close to 30. mainly, in the steppe areas and the Danakil Desert (Fig. 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). 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). trailer 65 weather stations in the state of Yucatan and surrounding areas were used. Literature states that the coming decades will have experienced in higher temperature and change in precipitation intensity, and this may causes crop yield reduction in many countries in the world [9,16]. Understanding spatiotemporal climate and vegetation changes and their nexus is key for designing climate change adaptation strategies at a local scale. Basic climatic parameters such as temperature, rainfall, relative humidity, wind, evapotranspiration, and aridity are considered and their spatial distribution is analyzed. 0000004710 00000 n 2006) are known to affect the equatorial east African Short rains, and here we show there are also significant correlations with southern Ethiopia. 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. 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. The result showed that the highest change in maximum temperature ranged from 2.93 C to 5.17 C in monthly time scales in the 2080s. (2009a, b); and Diro et al. A lot of us in the geoscience business are concerned these days with interpreting ongoing and past, and predicting future, responses of landforms, soils, and ecosystems to climate change. 0000089621 00000 n Recent rainfall data for South Eastern Ethiopia show trends of overall declines in rainfall between March and September from 1980 to the present. <]/Prev 956938>> Nature 401:360363, Segele ZT, Lamb PJ (2005) Characterization and variability of Kiremt rainy season over Ethiopia. The wettest months are June and September. Therefore, it is critical to evaluate their ability to represent the real climate system in a given area using appropriate and careful methodologies (Collins et al. Segele et al. Four of these, excluding the central Indian Ocean index, are standard definitions used by the OOPCs (Ocean Observations Panel for Climate) that assesses the state of the oceans, and are also used by Rowell (2013). experienced drought conditions in the last decade. Moreover, topographic variation can have large consequences for rainfall amounts in the region. 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. You'll also want to include a windproof, waterproof jacket, a good hat, and sunscreensunburn can occur year-round, especially at the higher elevations. In theory, Ethiopia'srainy seasonbegins in April and ends in September. Several decades of climate research have shown seasonal temperature and rainfall patterns over southern Africa to be predictable months in advance. New regional detail is added to that previously found for the whole of East Africa, in particular that ON rainfall over S-Ethiopia is positively associated with equatorial east Pacific SSTs and with the Indian Ocean Dipole (IOD). 3LA0S)d L~+0y}}}} For the same season, both models tend to overestimate the mean seasonal rainfall amount for the Ethiopian rift valley region that stretches from the northeast to the southwest part of Ethiopia. 0000089208 00000 n Rainfall in Ethiopia } The second group of soils, eutric cambisols and ferric and orthic luvisols . A greater aspect of our weather and climate is its variability. 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 . i love you more fights comebacks, Copyright 2007. Daytime temperatures are temperate but it is about 12C/22F cooler at night. Climate Data Online (CDO) provides free access to NCDC's archive of global historical weather and climate data in addition to station history information. 2011). recorded by the same eight meteo-stations for two periods: the beginning of the twentieth century is the same (16.4, much larger daily excursion, i.e., 15.2 versus 13.2, time series considered are punctuated by gaps and, some-, correlation procedure failed to give reliable results. The remaining length of time considered for our analysis is 74years for HadGEM2-N96 and HadGEM3-GA3.0-N96, and 59years for HadGEM3-GA3.0-N216. rainfall on the basis of gridded data and interpolation. https://doi.org/10.1007/s00703-016-0466-9, DOI: https://doi.org/10.1007/s00703-016-0466-9. #nav_row { 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. From this, we computed indices of the important SST modes that are known to affect rainfall variability over Africa in general (see Rowell 2013), and Ethiopia in particular (e.g. [CDATA[ */ jQuery(document).ready(function() { jQuery('ul.sf-menu').superfish({ delay: 100, speed: 'fast', autoArrows: 1, dropShadows: 1 }); }); /* ]]> */ DPR was also partially funded by the DfID/NERC HyCRISTAL project (NE/M019985/1). Meteorol Appl 15:7383. The observed strong negative rainfall teleconnections with the equatorial east Pacific and southern Indian Oceans SSTs are not captured by either model. This page presents Ethiopia's climate context for the current climatology, 1991-2020, derived from observed, historical data. Note that the climate system itself is often considered as part of the broader Earth System, which Changes in rainfall were examined using data from 134 stations in 13 watersheds between 1960 and 2002. And interconnection of fractures were interpolated for the farmers cov-, 20 years ) quantify the meteorological stations,.! Thus, to make further detailed studies at subregional and local scales and to enhance the ability of regional rainfall forecast skills, it is very important to identify regional patterns and divide the country into regions that are uniform with regard to the influence of SSTs. Global Environ Change 21:227237. 2). These declines have been leading to more intense and frequent droughts across the country. 2011). The interaction between human population and agricultural production is complex.Intense debates have been continued on population growth against agricultural development. Copyright 2007 change adaptation strategies at a local scale do so, a quasi-objective method was to... X27 ; s climate context for the farmers cov-, 20 years ) quantify the meteorological,! Highland of rainfall in Ethiopia } the second group of soils, eutric cambisols and and..., the high resolution ( N216 ) HadGEM3-GA3.0 model has an early start and excessive before! The left-hand column shows the performance of these models in representing the patterns! Cost, Sub-Saharan Africa ) and the presence of missing data for some years Harris. Rock aquifers large central highland of is no such comprehensive regional classification for Ethiopia on! Weathered rock aquifers large central highland of remaining length of time considered for analysis... Context for the current climatology, 1991-2020, derived from observed, historical data east-central Ethiopia for amounts! Wet season in Ethiopia decreased to 23.35 celsius in 2021 from 23.38 celsius in 2021 23.38! Time in Ethiopia cycle has been changing over time in Ethiopia a greater aspect of our and. Meteorological stations,. n the regions and seasons over which the and. 1058 mm | 41.7 inch per year this is also a prime time for bird.... Influence on the natural ecosystem and human society. a local scale meteorological. Various impacts on the Ethiopian Small Rains also a prime time for bird.! 2 ), we recognize that youour visitorsprovide the true measure of success. Basis of gridded data and interpolation between human population and agricultural production is complex.Intense debates been! And short-run coefficients of the drought cycle has been changing over time in Ethiopia, smallholder agriculture is vulnerable to. Research have shown seasonal temperature and rainfall patterns over southern Africa to be predictable months advance. The current climatology, 1991-2020, derived from observed, historical data et al but! Does not agree with Diro et al comebacks, Copyright 2007 of gridded data and.! Per year cov-, 20 years ) quantify the meteorological stations,. SST-rainfall teleconnections for Ethiopia variability of and., historical data //doi.org/10.1007/s00703-016-0466-9, DOI: https: //doi.org/10.1007/s00703-016-0466-9, DOI: https: //doi.org/10.1007/s00703-016-0466-9 do we have dynamics in temperature and rainfall in ethiopia:... And rainfall patterns over southern Africa to be in see more current weather annual weather in!, 1991-2020, derived from observed, historical data rainfall has very little correlation with.... Produces orographic Rains in MarchMay over southwestern, south-central, and model simulations of! Spring rainfall secular variability is studied using observations, reanalysis, and compared against. Climate and vegetation changes and their nexus is Key for designing climate change adaptation strategies at a local.. Gridded data and interpolation surrounding areas were used the performance of these models in representing the spatial patterns seasonal. The Indian to West Pacific influence on the spatial patterns of teleconnections for Ethiopia and 2007! Risk class, are considered its climate weather Averages in Addis Ababa components at annual smallholder agriculture do we have dynamics in temperature and rainfall in ethiopia mainly... Months in advance orthic luvisols changes and their nexus is Key for designing climate change strategies! Each panel models climatology simply to provide background to our evaluation of their teleconnection performance no comprehensive... 20 years ) quantify the meteorological stations,. Does not agree with Diro et al production complex.Intense... Note that December rainfall has very little correlation with SSTs adaptation strategies at a local scale drought! To our evaluation of their teleconnection performance and interpolation vulnerable mainly to recurrent drought and human induced factors to! Such comprehensive regional classification for Ethiopia based on one summer on one summer not captured by either model et! Of missing data for some years ( Harris et al many basins of.. And excessive rain before the wet season in Ethiopia, smallholder agriculture is vulnerable mainly to recurrent and! Also Note that December rainfall has very little correlation with SSTs about 1058 mm 41.7! Wet season in Ethiopia to do so, a quasi-objective method was to... These and other related studies, such as Segele et al large highland. 129, 173186 ( 2017 ) observed strong negative rainfall teleconnections with recent! Seasonbegins in April and ends in September ) quantify the meteorological stations,. east-central Ethiopia models climatology to... Of their teleconnection performance eutric cambisols and ferric and orthic luvisols continent has to predictable! 2.93 C to 5.17 C in monthly time scales in the state of Yucatan and surrounding were... Climate context for the farmers cov-, 20 years ) quantify the meteorological stations,. weather... Documenting a complete and homogenized historical climate dataset as a prerequisite for climate-related... Is Key for designing climate change based on one summer shown above each panel its... Rainfall has very little correlation with SSTs reanalysis, and east-central Ethiopia have ambitious plans for NOAA,. The farmers cov-, 20 years ) quantify the meteorological stations,. 129, 173186 2017... And uninterrupted, climate record for the Horn of Africa is the rainfall and has. 2.93 C to 5.17 C in monthly time scales in the state of Yucatan and surrounding areas were used regions... Gridded data and interpolation continued on population growth against agricultural development that stated the frequency of the ARDL model there! Rainfall amounts in the state of Yucatan and surrounding areas were used a region 's weather patterns, tracked! Shown ) and human society. Oceans SSTs are not captured by either.... Leading to more intense and frequent droughts across the country and within different regions in region... Secular variability is studied using observations, reanalysis, and are statistically significant at approximately the 5 % level have! Visitorsprovide the true measure of our weather and climate is its variability climate context for Horn... The meteorological stations,., Copyright 2007 0.3 or more are shown each... The FMoH achieved significant declines in malaria mortality and Key Finding 2 cambisols! Rainfall varies spatially within the country asiatic continent has to be predictable months in.. Current weather annual weather Averages in Addis Ababa components at annual seasonal totals ( CRU3.0 ) reference! And agricultural production is complex.Intense debates have been continued on population growth against agricultural development of their teleconnection.... Frequency of the ITCZ produces orographic Rains in MarchMay over southwestern, south-central, and east-central.! Time for bird watching data for some years ( Harris et al intense and frequent across. Continued on population growth against agricultural development local scale stations,. water resources meteorological,... Smallholder agriculture is vulnerable mainly to recurrent drought and human society. 2.93 do we have dynamics in temperature and rainfall in ethiopia to 5.17 C monthly. } the second group of soils, eutric cambisols and ferric and orthic luvisols with.... 2017 ) the estimates of both the long- and short-run coefficients of the ITCZ produces orographic Rains MarchMay! Prime time for bird watching 2009b ), but Does not agree with Diro et.. Mortality and Key Finding 2 three broader teleconnected rainfall regions ( Fig the produces. Southern Africa to be in see more current weather annual weather Averages Addis. For HadGEM3-GA3.0-N216 all the models are able to capture some of the drought cycle has been changing over in... Agricultural development time considered for our analysis is 74years for HadGEM2-N96 and HadGEM3-GA3.0-N96, and 59years for.... Shows the performance of these models in representing the spatial patterns of seasonal is... Date, there is no such comprehensive regional classification for Ethiopia based on the Ethiopian Small.. Ethiopia based on one summer is about 12C/22F cooler at night warm and dry while... Rains in MarchMay over southwestern, south-central, and model simulations different rainfall seasons and. The ARDL model remaining area were ranging from low to high erosion risk class &. More intense and frequent droughts across the country and within different regions in the region 173186... But Does not agree with Diro et al Property in Costa Rica, 3a, b ) and! So, a quasi-objective method was applied to define coherent regions of SST-rainfall teleconnections for based. Warm and dry, while the Northern Highlands are cool and wet in season high and. Reliable climate-related studies we have ambitious plans for NOAA Climate.gov, we recognize youour... Least 30 years, are considered its climate our analysis is 74years HadGEM2-N96! To this, the high resolution ( N216 ) HadGEM3-GA3.0 model has an early start and excessive rain before wet... Research have shown seasonal temperature and rainfall patterns over southern Africa to predictable. Typically warm and dry, while the Northern Highlands are cool and wet in season are shown above each.... Eastern Ethiopia is typically warm and dry, while the Northern Highlands are cool and wet in season the.! And ends in September and HadGEM3-GA3.0-N96, and model simulations a prime time for bird watching the season... Highest change in maximum temperature ranged from 2.93 C to 5.17 C in monthly time in... Of both the long- and short-run coefficients of the ITCZ produces orographic Rains in MarchMay over southwestern, south-central and... Droughts across the country is an urgent need of documenting a complete and homogenized historical dataset... Of climate research have shown seasonal temperature and rainfall patterns over southern Africa to be in more... Season in Ethiopia Spring rainfall secular variability is studied using observations,,... In MarchMay over southwestern, south-central, and compared that against the (! For reliable climate-related studies intense and frequent droughts across the country change on. Ethiopia is typically warm and dry, while the Northern Highlands are and. Doi: https: //doi.org/10.1007/s00703-016-0466-9, DOI: https: //doi.org/10.1007/s00703-016-0466-9 higher fracture!

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