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.

Aerosol microphysics simulations of the Mt.~Pinatubo eruption with the UM-UKCA composition-climate model

We use a stratosphere–troposphere composition–climate model with interactive sulfur chemistry and aerosol microphysics, to investigate the effect of the 1991 Mount Pinatubo eruption on stratospheric aerosol properties. Satellite measurements indicate that shortly after the eruption, between 14 and 23 Tg of SO2 (7 to 11.5 Tg of sulfur) was present in the tropical stratosphere. Best estimates of the peak global stratospheric aerosol burden are in the range 19 to 26 Tg, or 3.7 to 6.7 Tg of sulfur assuming a composition of between 59 and 77 % H2SO4. In light of this large uncertainty range, we performed two main simulations with 10 and 20 Tg of SO2 injected into the tropical lower stratosphere. Simulated stratospheric aerosol properties through the 1991 to 1995 period are compared against a range of available satellite and in situ measurements. Stratospheric aerosol optical depth (sAOD) and effective radius from both simulations show good qualitative agreement with the observations, with the timing of peak sAOD and decay timescale matching well with the observations in the tropics and mid-latitudes. However, injecting 20 Tg gives a factor of 2 too high stratospheric aerosol mass burden compared to the satellite data, with consequent strong high biases in simulated sAOD and surface area density, with the 10 Tg injection in much better agreement. Our model cannot explain the large fraction of the injected sulfur that the satellite-derived SO2 and aerosol burdens indicate was removed within the first few months after the eruption. We suggest that either there is an additional alternative loss pathway for the SO2 not included in our model (e.g. via accommodation into ash or ice in the volcanic cloud) or that a larger proportion of the injected sulfur was removed via cross-tropopause transport than in our simulations. We also critically evaluate the simulated evolution of the particle size distribution, comparing in detail to balloon-borne optical particle counter (OPC) measurements from Laramie, Wyoming, USA (41° N). Overall, the model captures remarkably well the complex variations in particle concentration profiles across the different OPC size channels. However, for the 19 to 27 km injection height-range used here, both runs have a modest high bias in the lowermost stratosphere for the finest particles (radii less than 250 nm), and the decay timescale is longer in the model for these particles, with a much later return to background conditions. Also, whereas the 10 Tg run compared best to the satellite measurements, a significant low bias is apparent in the coarser size channels in the volcanically perturbed lower stratosphere. Overall, our results suggest that, with appropriate calibration, aerosol microphysics models are capable of capturing the observed variation in particle size distribution in the stratosphere across both volcanically perturbed and quiescent conditions. Furthermore, additional sensitivity simulations suggest that predictions with the models are robust to uncertainties in sub-grid particle formation and nucleation rates in the stratosphere.

Avaliação da qualidade de vida dos funcionários do cartório do 1º Ofício da cidade de Diamantino-MT através do questionário SF-36

O objetivo desta pesquisa foi analisar a qualidade de vida dos funcionários do Cartório de 1º Ofício da cidade de Diamantino, em Mato Grosso. Foi utilizada a versão brasileira do Short Form-36 (SF-36) em dez funcionários do Cartório de 1º Ofício, que colaboraram voluntariamente para a coleta da análise dos dados do questionário. O estudo obteve a análise dos oito domínios do escore do SF-36, onde pôde ser observado que o primeiro domínio, relativo à capacidade funcional, foi aquele que apresentou o maior escore, enquanto os demais domínios (D2, D3, D4, D5, D6, D7 e D8), respectivamente relacionados à saúde mental, também estão acima da metade do valor máximo esperado no escore do SF-36. O questionário SF-36 foi um instrumento adequado, de aplicação relativamente rápida e de fácil uso para a avaliação da qualidade de vida dos funcionários do Cartório de 1º Ofício, pois, na amostra estudada, os oito domínios apresentaram resultado médio entre 51,9 (menor escore = domínio 4) e 71,8 (maior escore = domínio 1).

Na fronteira : os atuais dilemas da escola indígena em aldeias Paresi de Tangará da Serra-MT, num olhar dos Estudos Culturais

O presente trabalho apresenta algumas reflexões, de inspiração nos Estudos Culturais, a partir de análise textual de vozes indígenas, sobre os atuais dilemas da escola indígena em aldeias Paresi de Tangará da Serra-MT, tendo em vista a alternativa de se propor um modelo de escolarização formal, de valorização à diferença frente ao atual modelo de princípios homogeneizantes. Utilizando-se de conceitos de Stuart Hall, Nestor Canclini e outros autores pós-estruturalistas, discute-se a cultura numa perspectiva dinâmica de movimento contínuo de (re)construções de identidades, principalmente sob efeitos do fenômeno da globalização, quando o avanço da tecnologia da comunicação e transporte permitem, com maior freqüência, as relações e os fluxos migratórios entre as diversas culturas construindo identidades e culturas híbridas. A partir da discussão sobre como os Paresi entendem a função da escola da aldeia amplia-se a reflexão sobre a valorização da língua portuguesa nas rotinas escolares, assim como a relevância do comportamento disciplinar dos alunos daquelas escolas.

Formação de professores : um olhar sobre a pesquisa educacional como espaço curricular em ação : UNEMAT - Sinop/MT

Esta dissertação objetiva compreender a relevância e as contribuições da Disciplina Pesquisa Educacional, definida como elemento integrador e teorizador das práticas pedagógicas, da formação de professor do Curso de Pedagogia da Universidade do Estado de Mato Grosso - Campus de Sinop. Para tal intento lança um olhar sobre seu currículo, implantado em 1997, para verificar em que medida os propósitos desta disciplina, definida como eixo curricular, foram ou estão sendo alcançados. Para tanto, este estudo percorre a trajetória acerca da formação inicial de professores enfatiza a função da universidade e o papel da pesquisa como elemento formador na graduação no contexto brasileiro. Realiza um estudo teórico sobre a formação de professores e sobre o currículo; mostra suas vertentes e define o nível do currículo em ação como possibilidade de compreender o alcance e os propósitos da disciplina. É uma pesquisa com enfoque qualitativo, seguindo referenciais do estudo de caso e envolve como sujeitos, professores universitários, alunos e egressos do curso de Pedagogia de Sinop. Também realiza uma análise documental do currículo que iniciou em 1990; da proposta curricular reformulada; das produções monográficas dos seus alunos e seus egressos. O resultado deste estudo revela que a disciplina Pesquisa Educacional é espaço curricular privilegiado para se promover a integração dos conhecimentos e teorizar as práticas pedagógicas mediadas por atividades e/ou tarefas acadêmicas que são elos entre os pressupostos teóricos e a ação.

Programa Nacional de Educação na Reforma Agrária : o caso do curso "Pedagogia da Terra" da Universidade do Estado de Mato Grosso, Cáceres/MT

O principal objetivo da pesquisa Programa Nacional de Educação na Reforma Agrária: o caso do curso Pedagogia da Terra da UNEMAT é analisar a experiência do convênio do curso Pedagogia da Terra, realizado no período de julho de 1999 a julho de 2003, focalizando as relações entre os sujeitos sociais envolvidos, principalmente entre a UNEMAT e o MST, também incluindo instituições e órgãos governamentais. A pesquisa é de abordagem qualitativa e faz uma análise histórica das lutas de resistência camponesa no Brasil e das mais recentes ações do MST na luta por terra e por Reforma Agrária. Analisa articulações com outros sujeitos sociais e entidades da sociedade civil em busca de políticas públicas de educação do campo, resultando no Programa Nacional de Educação na Reforma Agrária em 1998 e na possibilidade de se desenvolverem ações nessa área, em parcerias com universidades, instituições e órgãos governamentais. A pesquisa, que levou em conta o contexto de crise do capitalismo e de reforma do Estado no Brasil a partir dos anos de 1990, foi conduzida através de análise documental e bibliográfica e entrevistas semi-estruturadas. Os resultados apontaram para alguns avanços, limites e contradições relacionados com os aspectos metodológicos, de gestão e de financiamento, também indicando relações entre as tendências teórico-metodológicas do Projeto Político Pedagógico do curso e aquelas que influenciam os trabalhos educativos do MST. Este estudo pode contribuir para subsidiar políticas educacionais resultantes de projetos em parcerias hoje no país.