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

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.

2020 ◽  
Vol 52 (2) ◽  
pp. 341-348
Author(s):  
Thomas Cassar

This study presents a species account of the mantises of the Maltese Islands, including notes on the ecology and distribution of each species. A total of three species are known to exist locally; Ameles spallanzania (Rossi, 1792), Mantis religiosa (Linnaeus, 1758) and Rivetina baetica Rambur, 1839. The presence of Ameles decolor (Charpentier, 1825) cannot be confirmed by any recently collected material, but the species is not excluded from the Maltese entomofauna. Two doubtful records are also discussed. All species present in the archipelago are typically found in Southern Europe and the Mediterranean basin.


Wine Studies ◽  
2011 ◽  
Vol 1 (1) ◽  
pp. 1
Author(s):  
Maurizio Trevisan

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.


2020 ◽  
Author(s):  
Manfred A. Lange

<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>


2010 ◽  
Vol 41 (4) ◽  
pp. 270-280 ◽  
Author(s):  
N. Luchi ◽  
D. Paffetti ◽  
K. Korhonen ◽  
J. Hantula ◽  
P. Capretti

2014 ◽  
Vol 14 (7) ◽  
pp. 9975-10024
Author(s):  
P. Ricaud ◽  
B. Sič ◽  
L. El Amraoui ◽  
J.-L. Attié ◽  
P. Huszar ◽  
...  

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.


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