scholarly journals Gender Issue and Water Management in the Mediterranean Basin, Middle East and North Africa

2007 ◽  
Author(s):  
Giulia Minoia
Keyword(s):  
Water Management ◽  
Middle East ◽  
North Africa ◽  
Mediterranean Basin ◽  
Gender Issue ◽  
The Mediterranean ◽  
The Mediterranean Basin

The Water-Energy Nexus in the Middle East and North Africa under Climate Change

2020 ◽  
Author(s):  
Manfred A. Lange
Keyword(s):  
Climate Change ◽  
Middle East ◽  
North Africa ◽  
Mediterranean Basin ◽  
Mena Region ◽  
Mena Countries ◽  
Water Energy Nexus ◽  
The Mediterranean ◽  
The Mediterranean Basin ◽  
Impacts Of Climate Change

<p>The region of the Middle East and North Africa (MENA region) encompasses countries of the eastern Mediterranean, the Middle East, and North Africa, from Morocco in the West to the Islamic Republic of Iran in the East and from the Syrian Arab Republic in the North to the Republic of Yemen in the South. It is home to some 500 million inhabitants and is characterized by widely varied political and economic settings and a rich cultural heritage. Stark environmental gradients, as well as significant differences in the provision of ecosystem services, both East to West and South to North, are typical for the MENA Region.</p><p>Climate changes in the Mediterranean Basin, in general, and in the MENA countries, in particular, currently exceed global mean values significantly. Numerical model results indicate that this trend will continue in the near future and imply that the number of extreme summer temperatures and heatwaves may increase significantly over the coming decades. At the same time, a decrease in precipitation and a significantly longer dry season for most MENA countries than at present are anticipated. This leads to a significantly increased demand for water and energy. In addition, other factors further exacerbate these demands in the MENA, including the general economic development, extreme population growth and increasing urbanization, changes in lifestyle, shifting consumption patterns, inefficiencies in the use of resources that result from technical and managerial inadequacies and energy and water subsidies in several countries of the region to name but a few.</p><p>The impacts of climate change will be particularly severe in urban settings and large cities of the Mediterranean Basin and the MENA region. Cities will see an enhanced heat accumulation compared to the surrounding rural land due to heat-build-up in buildings, transportation infrastructure, and enhanced human activities. Reduced ventilation within cities exacerbates the warming, particularly during summer heatwaves. Consequently, additional, energy-intensive space cooling will be needed in order to maintain acceptable indoor conditions. With regard to water scarcity, the aforementioned decreases in precipitation will reduce available drinking water for city inhabitants and green spaces. This requires the provision of unconventional water sources, e.g., through desalination, which requires significant quantities of energy. Overall, climate change will exacerbate resource demand for water and energy, in general, and in urban settings, in particular.</p><p>However, the provision of water and energy are interrelated. In order to maintain water and energy security in the MENA region, these issues need therefore be considered holistically in the framework of the Water-Energy-Nexus (WEN).</p><p>The present paper aims to elucidate some of the interrelationships between water and energy resources and their provision and will briefly outline a few of the possible mitigation/adaptation options/strategies to reduce adverse impacts of climate change on the MENA region and its inhabitants.</p>

scholarly journals Xylella fastidiosa invasion of new countries in Europe, the Middle East and North Africa: Ranking the potential exposure scenarios

NeoBiota ◽  
2020 ◽  
Vol 59 ◽  
pp. 77-97 ◽  
Author(s):  
Michel Frem ◽  
Daniel Chapman ◽  
Vincenzo Fucilli ◽  
Elia Choueiri ◽  
Maroun El Moujabber ◽  
...  
Keyword(s):  
Middle East ◽  
North Africa ◽  
Mediterranean Basin ◽  
Xylella Fastidiosa ◽  
European Countries ◽  
Summer Temperatures ◽  
The Mediterranean ◽  
High Level ◽  
The Mediterranean Basin ◽  
Level Of Risk

After the recent high-impact European outbreaks of Xylella fastidiosa (Xf), a xylem-limited plant pathogenic bacterium native to the Americas, this research aims to rank the risks of potential entry, establishment and spread of Xf in new countries across Europe, the Middle East and North Africa. A novel risk-ranking technique is developed, based on combining entry risk drivers (imported plants, direct flights and ferry connections) with risk factors related to establishment and spread (presence of potential insect vectors, vulnerable economic crops, alternative hosts and climate suitability) of this pathogen. This reveals that western European countries have the highest risk for entry, but that the Mediterranean basin runs the highest risk for establishment and spread of Xf. Lebanon in particular has the highest level of risk for Xf dispersal within its suitable territory. Countries without current outbreaks combining high risks of Xf arrival and establishment are mainly in the Mediterranean basin: Turkey is at the highest level of risk, followed by Greece, Morocco and Tunisia, which are ranked at the high level. The ranking model also confirms the vulnerability, in terms of invasion by Xf, of southern European countries (Italy, Portugal and Spain) in which the pathogen has already been reported. High summer temperatures in these southern countries are likely to be the significant determinant for the overall invasion process, while northern European countries have a high level risk for the arrival of the pathogen, but relatively low summer temperatures may limit establishment and spread of major outbreaks. In general, our study provides a useful approach for mapping and comparing risks of invasive non-native species and emerging pathogens between countries, which could be useful for regional horizon scanning and phytosanitary and biosecurity management.

scholarly journals Wine and Society - Welcome Editorial

Wine Studies ◽  
2011 ◽  
Vol 1 (1) ◽  
pp. 1
Author(s):  
Maurizio Trevisan
Keyword(s):  
Middle East ◽  
Mediterranean Basin ◽  
Ancient Egypt ◽  
Early Sign ◽  
Western Civilization ◽  
Nile Valley ◽  
Production And Consumption ◽  
Fertile Crescent ◽  
The Mediterranean ◽  
The Mediterranean Basin

Wine, its production and consumption, has accompanied western civilization for thousands of years. Since the early sign of its production in the Fertile crescent area, approximately 6000-8000 years ago, the culture of wine has spread out through the middle east, the Nile valley and the Mediterranean basin. Wine became part of the recorded history in ancient Egypt were it was used as part of religious ceremonies and by the Pharaos and the elite.

Rabbis with Inky Fingers : Making An Eighteenth-Century Hebrew Book Between North Africa and Amsterdam

2020 ◽  
Vol 46 (1) ◽  
pp. 155-187
Author(s):  
Noam Sienna
Keyword(s):  
Eighteenth Century ◽  
North Africa ◽  
Mediterranean Basin ◽  
18Th Century ◽  
Book Production ◽  
Jewish Communities ◽  
The Press ◽  
The Mediterranean ◽  
The Mediterranean Basin ◽  
Manuscript Copy

Abstract The first edition of Sefer Hatashbe, a collection of responsa printed in Amsterdam in 1739 at the press of Naftali Herz Levi Rofé, is a magnificent example of the fine typography and engraving that contributed to the prominence of 18th-century Dutch Jewish printing. Through an examination of the newly identified manuscript copy which was used in the printing house to typeset this book, I trace the story of the printing of Sefer Hatashbe through the efforts of Meir Crescas of Algiers, and his collaboration with Ashkenazi, Sephardi, Maghrebi, and Italian Jewish communities. I demonstrate how the material facets of book production both relied on and reinforced the various networks ‐ intellectual, financial, religious, communal, familial, social ‐ that linked Jewish communities around the Mediterranean Basin and beyond, across class, nationality, and language.

scholarly journals Cultivation of Vitis vinifera L. in the light of former publications and today in Poland

2014 ◽  
Vol 67 (3) ◽  
pp. 3-12
Author(s):  
Krystyna Pudelska ◽  
Margot Dudkiewicz ◽  
Paweł Krawiec
Keyword(s):  
Middle East ◽  
Vitis Vinifera ◽  
Middle Ages ◽  
Mediterranean Basin ◽  
Ornamental Plant ◽  
Vitis Vinifera L ◽  
Southern Europe ◽  
Ancient Civilizations ◽  
The Mediterranean ◽  
The Mediterranean Basin

In the countries of the Mediterranean Basin viticulture has been dealt with for centuries. It was known to the ancient civilizations of the Middle East and grapevines were widely planted in Greece and Rome. The vineyard was part of the utility garden, usually occupying large areas and at the same time being a connection with the landscape. Creeper vine was also used in decorative gardens as an ornamental plant for various types of buildings and garden structures. The Polish tradition of planting vineyards dates back to the Middle Ages and is mainly associated with the activities of monks, although it was not as common as in the countries of southern Europe. However, in Polish gardening literature and in the literature that describes the development of the art of gardening, you can find lots of tips on how to grow grapevines, their varieties and the descriptions of the vineyards.

scholarly journals Variability of tropospheric methane above the Mediterranean Basin inferred from satellite and model data

2014 ◽  
Vol 14 (7) ◽  
pp. 9975-10024
Author(s):  
P. Ricaud ◽  
B. Sič ◽  
L. El Amraoui ◽  
J.-L. Attié ◽  
P. Huszar ◽  
...  
Keyword(s):  
Middle East ◽  
Atlantic Ocean ◽  
Mediterranean Basin ◽  
Near Infrared ◽  
Asian Monsoon ◽  
Transport Model ◽  
Emission Scenarios ◽  
The West ◽  
The Mediterranean ◽  
The Mediterranean Basin

Abstract. The space and time variabilities of methane (CH4) total column and upper tropospheric mixing ratios are analyzed above the Mediterranean Basin (MB) as part of the Chemical and Aerosol Mediterranean Experiment (ChArMEx) programme. Spaceborne measurements from the Thermal And Near infrared Sensor for carbon Observations-Fourier Transform Spectrometer (TANSO-FTS) instrument on the Greenhouse gases Observing SATellite (GOSAT) satellite, the Atmospheric InfraRed Spectrometer (AIRS) on the AURA platform and the Infrared Atmospheric Sounder Interferometer (IASI) instrument aboard the MetOp-A platform are used in conjunction with model results from the Chemical Transport Model (CTM) MOCAGE, and the Chemical Climate Models (CCMs) CNRM-AOCCM and LMDz-OR-INCA (according to different emission scenarios). In order to minimize systematic errors in the spaceborne measurements, we have only considered maritime pixels over the MB. The period under interest spans from 2008 to 2011 considering satellite and MOCAGE data and, regarding the CCMs, from 2001 to 2010. An East-West gradient in CH4 is observed and modelled whatever the season considered. In winter, air masses mainly originating from Atlantic Ocean and Europe tend to favour an elevated amount of mid-to-upper tropospheric CH4 in the West vs. the East of the MB, with a general upward transport above the MB. In summer, the meteorological state of the MB is changed, favouring air from Northern Africa and Middle East together with Atlantic Ocean and Europe, with a general downward motion above the MB. The Asian Monsoon traps and uplifts high amounts of CH4 that are transported towards North Africa and Middle East by the Asian Monsoon Anticyclone to finally reach and descent in the East of the MB. Consequently, the mid-to-upper tropospheric CH4 is much greater in the East than in the West of the MB. The seasonal variation of the difference in CH4 between the East and the West MB does show a maximum in summer for pressures from 500 to 100 hPa considering both spaceborne measurements and model results whatever the emission scenarios used. From this study, we can conclude that CH4 in the mid-to-upper troposphere over the MB is mainly affected by long-range transport, particularly intense in summer from Asia. In the low-to-mid troposphere, the local sources of emission in the vicinity of the MB mainly affect the CH4 variability.

scholarly journals Scenarios in the development of Mediterranean cyclones

2007 ◽  
Vol 12 ◽  
pp. 59-65 ◽  
Author(s):  
M. Romem ◽  
B. Ziv ◽  
H. Saaroni
Keyword(s):  
Atlantic Ocean ◽  
North Africa ◽  
Mediterranean Basin ◽  
Western Europe ◽  
Winter Season ◽  
Sahara Desert ◽  
Sea Level Pressure ◽  
Mediterranean Cyclones ◽  
The Mediterranean ◽  
The Mediterranean Basin

Abstract. The Mediterranean is one of the most cyclogenetic regions in the world. The cyclones are concentrated along its northern coasts and their tracks are oriented more or less west-east, with several secondary tracks connecting them to Europe and to North Africa. The aim of this study is to examine scenarios in the development of Mediterranean cyclones, based on five selected winter seasons (October–March). We detected the cyclones subjectively using 6-hourly Sea-Level Pressure maps, based on the NCAR/NCEP reanalysis archive. HMSO (1962) has shown that most Mediterranean cyclones (58%) enter the Mediterranean from the Atlantic Ocean (through Biscay and Gibraltar), and from the south-west, the Sahara Desert, while the rest are formed in the Mediterranean Basin itself. Our study revealed that only 13% of the cyclones entered the Mediterranean, while 87% were generated in the Mediterranean Basin. The entering cyclones originate in three different regions: the Sahara Desert (6%), the Atlantic Ocean (4%), and Western Europe (3%). The cyclones formed within the Mediterranean Basin were found to generate under the influence of external cyclonic systems, i.e. as "daughter cyclones" to "parent cyclones" or troughs. These parent systems are located in three regions: Europe (61%), North Africa and the Red Sea (34.5%) and the Mediterranean Basin itself (4.5%). The study presents scenarios in the development of Mediterranean cyclones during the winter season, emphasizing the cyclogenesis under the influence of various external forcing. The large difference with respect to the findings of HMSO (1962) is partly explained by the dominance of spring cyclones generating in the Sahara Desert, especially in April and May that were not included in our study period.

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