Using the significant dust deposition event on the glaciers of Mt. Elbrus, Caucasus Mountains, Russia on 5 May 2009 to develop a method for dating and "provenancing" of desert dust events recorded in snow pack

A significant desert dust deposition event occurred on Mt. Elbrus, Caucasus Mountains, Russia on 5 May 2009, where the deposited dust later appeared as a brown layer in the snow pack. An examination of dust transportation history and analysis of chemical and physical properties of the deposited dust were used to develop a new approach for high-resolution “provenancing” of dust deposition events recorded in snow pack using multiple independent techniques. A combination of SEVIRI red-green-blue composite imagery, MODIS atmospheric optical depth fields derived using the Deep Blue algorithm, air mass trajectories derived with HYSPLIT model and analysis of meteorological data enabled identification of dust source regions with high temporal (hours) and spatial (ca. 100 km) resolution. Dust, deposited on 5 May 2009, originated in the foothills of the Djebel Akhdar in eastern Libya where dust sources were activated by the intrusion of cold air from the Mediterranean Sea and Saharan low pressure system and transported to the Caucasus along the eastern Mediterranean coast, Syria and Turkey. Particles with an average diameter below 8 μm accounted for 90% of the measured particles in the sample with a mean of 3.58 μm, median 2.48 μm. The chemical signature of this long-travelled dust was significantly different from the locally-produced dust and close to that of soils collected in a palaeolake in the source region, in concentrations of hematite. Potential addition of dust from a secondary source in northern Mesopotamia introduced uncertainty in the “provenancing” of dust from this event. Nevertheless, the approach adopted here enables other dust horizons in the snowpack to be linked to specific dust transport events recorded in remote sensing and meteorological data archives.

Using the significant dust deposition event on the glaciers of Mt. Elbrus, Caucasus Mountains, Russia on 5 May 2009 to develop a method for dating and provenancing of desert dust events recorded in snow pack.

A significant desert dust deposition event occurred on Mt. Elbrus, Caucasus Mountains, Russia on 5 May 2009, where the deposited dust later appeared as a brown layer in the snow pack. An examination of dust transportation history and analysis of chemical and physical properties of the deposited dust were used to develop a new approach for high-resolution provenancing of dust deposition events recorded in snow pack using multiple independent techniques. A combination of SEVIRI red-green-blue composite imagery, MODIS atmospheric optical depth fields derived using the Deep Blue algorithm, air mass trajectories derived with HYSPLIT model and analysis of meteorological data enabled identification of dust source regions with high temporal (hours) and spatial (ca. 100 km) resolution. Dust, deposited on 5 May 2009, originated in the foothills of the Djebel Akhdar in eastern Libya where dust sources were activated by the intrusion of cold air from the Mediterranean Sea and Saharan low pressure system and transported to the Caucasus along the eastern Mediterranean coast, Syria and Turkey. Particles with an average diameter below 8 μm accounted for 90% of the measured particles in the sample with a mean of 3.58 μm, median 2.48 μm and the dominant mode of 0.60 μm. The chemical signature of this long-travelled dust was significantly different from the locally-produced dust and close to that of soils collected in a palaeolake in the source region, in concentrations of hematite and oxides of aluminium, manganese, and magnesium. Potential addition of dust from a secondary source in northern Mesopotamia introduced uncertainty in the provenancing of dust from this event. Nevertheless, the approach adopted here enables other dust horizons in the snowpack to be linked to specific dust transport events recorded in remote sensing and meteorological data archives.

Desert dust deposition on Mt. Elbrus, Caucasus Mountains, Russia in 2009-2012 as recorded in snow and shallow ice core: high-resolution "provenancing", transport patterns, physical properties and soluble ionic composition

A record of dust deposition events between 2009 and 2012 on Mt. Elbrus, Caucasus Mountains derived from a snow pit and a shallow ice core is presented for the first time for this region. A combination of isotopic analysis, SEVIRI red-green-blue composite imagery, MODIS atmospheric optical depth fields derived using the Deep Blue algorithm, air mass trajectories derived using the HYSPLIT model and analysis of meteorological data enabled identification of dust source regions with high temporal (hours) and spatial (cf. 20–100 km) resolution. Seventeen dust deposition events were detected; fourteen occurred in March–June, one in February and two in October. Four events originated in the Sahara, predominantly in north-eastern Libya and eastern Algeria. Thirteen events originated in the Middle East, in the Syrian Desert and northern Mesopotamia, from a mixture of natural and anthropogenic sources. Dust transportation from Sahara was associated with vigorous Saharan depressions, strong surface winds in the source region and mid-tropospheric south-westerly flow with daily winds speeds of 20–30 m s−1 at 700 hPa level and, although these events were less frequent, they resulted in higher dust concentrations in snow. Dust transportation from the Middle East was associated with weaker depressions forming over the source region, high pressure centered over or extending towards the Caspian Sea and a weaker southerly or south-easterly flow towards the Caucasus Mountains with daily wind speeds of 12–18 m s−1 at 700 hPa level. Higher concentrations of nitrates and ammonium characterise dust from the Middle East deposited on Mt. Elbrus in 2009 indicating contribution of anthropogenic sources. The modal values of particle size distributions ranged between 1.98 μm and 4.16 μm. Most samples were characterised by modal values of 2.0–2.8 μm with an average of 2.6 μm and there was no significant difference between dust from the Sahara and the Middle East.

High-resolution provenance of desert dust deposited on Mt. Elbrus, Caucasus in 2009–2012 using snow pit and firn core records

The first record of dust deposition events on Mt. Elbrus, Caucasus Mountains derived from a snow pit and a shallow firn core is presented for the 2009–2012 period. A combination of isotopic analysis, SEVIRI red-greenblue composite imagery, MODIS atmospheric optical depth fields derived using the Deep Blue algorithm, air mass trajectories derived using the HYSPLIT model and analyses of meteorological data enabled identification of dust source regions with high temporal (hours) and spatial (ca. 20–100 km) resolution. Seventeen dust deposition events were detected; fourteen occurred in March–June, one in February and two in October. Four events originated in the Sahara, predominantly in northeastern Libya and eastern Algeria. Thirteen events originated in the Middle East, in the Syrian Desert and northern Mesopotamia, from a mixture of natural and anthropogenic sources. Dust transportation from Sahara was associated with vigorous Saharan depressions, strong surface winds in the source region and mid-tropospheric southwesterly flow with daily winds speeds of 20–30 m s−1 at 700 hPa level. Although these events were less frequent than those originating in the Middle East, they resulted in higher dust concentrations in snow. Dust transportation from the Middle East was associated with weaker depressions forming over the source region, high pressure centred over or extending towards the Caspian Sea and a weaker southerly or southeasterly flow towards the Caucasus Mountains with daily wind speeds of 12–18 m s−1 at 700 hPa level. Higher concentrations of nitrates and ammonium characterised dust from the Middle East deposited on Mt. Elbrus in 2009 indicating contribution of anthropogenic sources. The modal values of particle size distributions ranged between 1.98 µm and 4.16 µm. Most samples were characterised by modal values of 2.0– 2.8 µm with an average of 2.6 µm and there was no signifi- cant difference between dust from the Sahara and the Middle East.

The world of the Sumerian mother goddess : an interpretation of her myths

The present study is an interpretation of the two myths copied in the Old Babylonian period in which the Sumerian mother goddess is one of the main actors. The first myth is commonly called “Enki and Ninḫursaĝa”, and the second “Enki and Ninmaḫ”. The theoretical point of departure is that myths have society as their referents, i.e. they are “talking about” society, and that this is done in an ideological way. This study aims at investigating on the one hand which contexts in the Mesopotamian society each section of the myths refers to, and on the other hand which ideological aspects that the myths express in terms of power relations. The myths are contextualized in relation to their historical and social setting. If the myth for example deals with working men, male work in the area during the relevant period is discussed. The same method of contextualization is used regarding marriage, geographical points of reference and so on. Also constellations of mythical ideas are contextualized, through comparison with similar constellations in other Mesopotamian myths. Besides the method of contextualization, the power relations in the myths are investigated. According to this latter method, the categories at issue, their ranking, as well as their changed ranking, are noted. The topics of the myths are issues important for the kingship and the country, such as irrigation, trade, health and healing, birth, collective work, artisanry and rivalry. All these aspects are used in order to express what the power relations between the goddess Ninḫursaĝa/Ninmaḫ and the god Enki look like. The relations are negotiated and recalibrated, which leads to the goddess getting a lowered status. Part of the negotiations and recalibrations is gender behavior, which is related to historical developments in society. The present work points to the function of these myths as tools of recalibrating not only deities, but also men and women in society.

From despotism to democracy : reporting Iraq's January 2005 election in the Australian and Middle Eastern print media

It is only in recent times that the magnitude of Ancient Mesopotamia’s contribution to language, agriculture, modern thought and urbane society has begun to be understood. Most relevant to this study is the governance of Mesopotamia’s early city-states by a political system that Jacobsen has termed ‘Primitive Democracy’ where “…ultimate political power rested with a general assembly of all adult freemen” (Jacobsen, 1977; 128). Yet, despite this, the coverage of Iraq in the Western media since its creation at the end of the First World War and particularly since the first Gulf War, has tended towards Orientalism (Said, 1978) by trivialising this nation and thereby reinforcing the hegemony of the West over the ‘backward, barbaric’ East.

This paper examines this issue further by comparing and contrasting the representations of the Iraqi election of January 30, 2005 in four of Australia’s leading daily newspapers (The Australian, The Courier-Mail, The Age and The Sydney Morning Herald) with four Middle Eastern English language papers (The Daily Star from Lebanon, Andolu Agency and Dunya both based in Turkey, and the eponymous Kuwait Times). In essence, it finds that while the Australian media posits democracy as a Western concept and asserts a discourse of US hegemony, the Middle Eastern papers are more contemplative, focusing on the impact that this election could have throughout the region.

Democracy in Iraq : history, politics, discourse

This book proposes a significant reassessment of the history of Iraq, documenting democratic experiences from ancient Mesopotamia through to the US occupation. Such an analysis takes to task claims that the ‘West’ has a uniquely democratic history and a responsibility to spread democracy across the world. It also reveals that Iraq has a democratic history all of its own, from ancient Middle Eastern assemblies and classical Islamic theology and philosophy, through to the myriad political parties, newspapers and protest movements of more recent times. This book argues that the democratic history of Iraq could serve as a powerful political and discursive tool where the Iraqi people may come to feel a sense of ownership over democracy and take pride in endorsing it. This could go a long way towards mitigating the current conflicts across the nation and in stabilizing and legitimating its troubled democracy.

Taking an interdisciplinary approach and referring to some of the most influential critical theorists to question ideological assumptions about democracy and its history, this book will be useful to those interested in political and legal history, human rights and democracy.

The destruction of heritage in Iraq since 2003

Since the invasion of Iraq by coalition forces in 2003, Iraq has endured an extraordinary period of destruction of cultural heritage.

This has included the attack on the Iraq National Museum in the very earliest days of the war. Since then, Iraq’s Mesopotamian heritage has also been systematically smuggled out of the country while coalition forces have converted key sites such as the ancient city of Babylon into modern military bases.

This lecture will examine the recent fate of Iraq’s Mesopotamian heritage and discusses the urgent need for appropriate management and protection.

On the growth and reproductive biology of asp, Aspius vorax, population from the middle reaches of Euphrates river

Endemic asp, Aspius vorax, from the middle section of the Euphrates River flowing through eastern Syria were studied to determine the main characteristics of their population structure, morphological parameters and reproductive biology. Samples ranged between 0+ and 4+ years of age and were dominated by 2+ years old group. Total length (TL) ranged between 19 and 70 cm corresponding with 46 to 2824.5 g weight, respectively. Fish growth has isometric pattern and the overall sex ratio was unbiased. Seasonal changes in the condition factor were related with the water temperature as well as the spawning season. Annual cycle of gonadosomatic index (GSI) readings indicated that spawning season occur around March when fish longer than 36 cm can mate. Average pre-spawning GSI was greater in individuals older than 2 years. Meanwhile, female fecundity was highly related to TL and weight. These findings did not always concur with previous observations from other asp populations, mainly in southern and northern Mesopotamia. Our results highlighted basic biological aspects of the local population and indicated differences between populations which can assist in fisheries management, conservation and commercial culture of the investigated species.

Historical aspects of Belly Dance and its practice in Brazil

Dance is regarded as one of the oldest art forms, which is based on evidence from prehistoric paintings found in caves; man expressed himself through body language prior to the development of spoken and written forms of communication. Dance was then used during important events, common to their era and culture, and often in religious rituals, to ensure good harvests - their economic activity. Belly-dance appeared approximately eight thousand years B. C. E. as a sacred dance firstly practiced by priestesses, and after that, it was popularized amongst women from Mesopotamia. Virtually considered an ancient form of physical exercise, it is still practiced by Bedouin women as a preparation for spontaneous delivery. In Brazil, belly-dance is widely practiced and our corporal culture enables its learning and improvement, resulting in professional dancers.

Agricultura y cambio climático: instituciones, políticas e innovación. Memoria del seminario internacional realizado en Santiago, los días 10 y 11 de noviembre de 2010

Incluye Bibliografía

Análise de ocorrências dos impactos pluviais na área urbana de Rio Claro (SP)

The Urbanization is a notable process in our society, being part of it since around 3500 BC in Mesopotamia, currently Iraq area. Since the Industrial Revolution, cities had a significant increase in their growth and began to concentrate increasingly labor and capital. Brazil, despite having had a late industrialization, also had a high population growth in cities, especially in the XVIII century, which were not provided with any kind of planning that targets the ordering and implementation of the urban essential apparatus. Therefore, Brazilian cities started to exhibit countless structural and environmental problems. Associated with inadequate infrastructure, the modifications in the urban atmosphere, like increased heat, air pollution and increased rainfall and storm frequency, cause different types of impacts in cities. Among the most worrisome are those from the intense rain, which cause human and material damage. The city of Rio Claro (SP) can be considered an example of this reality. Thereby, the objective of this study was to analyze the impacts on the population originated from rainfall in the urban area during the period 2005-2010, by the mapping of events and analysis of the active atmospheric systems. The information of the events were collected in the Fire Department and the Press and the synoptic maps were obtained in the library of INPE, in Cachoeira Paulista (SP) and in the site of the Navy of Brazil. The data showed that among 247 occurrences, during the six years, 233 occurred in the spring-summer period. Moreover, after finalizing the maps, it was found the locations considered critical regarding the frequency of occurrences, as: Visconde do Rio Claro Avenue and central area of the city, both with a total of 23 occurrences; Jardim Inocoop, with 20; Tancredo Neves Avenue, with 12 and Vila Paulista, with 10 occurrences. Through the graphs, it was found that the most recurrent atmospheric system, during the studied period, is...

La inundación del Mar Negro. ¿Pudo haber sido ésta la inundación de Noé?

[ES] Entre 15 y 6 mil años atrás, durante la era del Neolítico, el nivel del Mar Mediterráneo subió entre 100 y 10 m. por debajo de su nivel actual. En esta época el Mar Negro era un lago de agua dulce (Lago Nuevo Euxino) que desembocaba en el Mar Egeo. Sin embargo, durante este periodo se fue secando poco a poco y el nivel de su superficie descendió a 150 mmetros por debajo de su nivel actual. Hace 7.150 años, tal vez gracias a la ayuda de un terremoto, el mar rompió el dique del Bósforo que separaba el Lago Nuevo Euxino del Mar Egeo. En un principio fue una pequeña corriente de agua salada que fluía a través del valle del Bósforo hacia el lago, pero en poco tiempo ésta se convirtió en un torrente y luego en un diluvio. Fue tanta la cantidad de agua salada que fluía a través del Bósforo que el nivel del lago subía ventricuatro centrímetros por día y se llenó en tan sólo dos años. Debido a esta inundación, los valles se convirtieron en trampas mortales y las personas que vivían en la periferia del lago se vieron obligados a evacuar sus hogares y ciudades y trasladarse a terrenos más altos, escapando hacia Europa, India, Mesopotamia, Armenia, Anatolia y Grecia. Algunos historiadores sostienen que los refugiados que llegaron a Egipto comenzaron la leyenda de la Atlántida. Según los profesores Ryan y Pitman, descubridores de la inundación del Mar Negro, todos los habitantes de esta diáspora hablaban un lenguaje similar, Indo-Europeo, y por ello explican las similitudes existentes entre el sánscrito, el alemán y el latín. Los profesores Ryan y Pitman proponen además en su libro que la inundación del Mar Negro, la devastación y la posterior diáspora es la base para el relato bíblico del Diluvio Univeral de Noé.

Materiale epigrafico per la ricostruzione dei contatti nel Mediterraneo tra il 1200 a.C. e il 500 a.C.

La Tesi Materiale epigrafico per la ricostruzione dei contatti nel Mediterraneo tra il 1200 a.C. e il 500 a.C. si propone di illustrare i complessi rapporti instauratisi tra i vari popoli che si affacciarono sulle rive del Mediterraneo e nelle sue vicinanze, tra il 1200 e il 500 a.C. circa, quali emergono dalle iscrizioni disponibili, principalmente greche e semitiche (soprattutto fenicie, ebraiche, aramaiche e assire), prendendo tuttavia in esame anche iscrizioni ittite, egiziane, frigie, etrusche e celtiche. Le date suddette riguardano due eventi cruciali, che sconvolsero il Mediterraneo: gli attacchi dei Popoli del Mare, che distrussero l'Impero Ittita e indebolirono l'Egitto, e le guerre Persiane. Le iscrizioni riportate sono 1546, quasi sempre traslitterate, tradotte, e accompagnate da un'immagine, da riferimenti bibliografici essenziali e da una breve motivazione del collegamento proposto. Il quadro che si delinea ben testimonia la complessità dei rapporti che si intrecciarono in quel periodo: si pensi alle centinaia di graffiti greci trovati a Naucrati, in Egitto, o alle decine di iscrizioni greche trovate a Gravisca. Anche le iscrizioni aramaiche e assire attestano gli stretti rapporti che si formarono tra Siria e Mesopotamia; ugualmente Iran e Arabia sono, direttamente o indirettamente, collegati a Etruria e Grecia; così troviamo un'iscrizione greca nel cuore dell'Impero Persiano, e un cratere laconico nel centro della Gallia. In realtà lo scopo di questo lavoro è anche quello di mettere in contatto due mondi sostanzialmente separati, ossia quello dei Semitisti e quello dei Grecisti, che solo apparentemente si conoscono e collaborano. Inoltre vorrei soavemente insinuare l'idea che la tesi di Joseph Naveh, che ipotizzò che gli alfabeti greci abbiano tratto origine in prima istanza dalle iscrizioni protocananaiche, nel XII sec. a.C., è valida, e che solo in un secondo tempo i Fenici abbiano dato il loro apporto.