Estudo da expansão de áreas de cana-de-açúcar na Bacia do Alto Paraguai.

O presente trabalho tem por objetivo analisar a expansão da área cultivada com cana-de-açúcar nessa bacia, no período de 2005 a 2009, e quais fisionomias foram convertidas

Distribuição de formações pioneiras no Pantanal brasileiro.

Em regiões alagáveis como o Pantanal, a alternância de períodos secos e cheios favorece o aparecimento de vegetação sob influência fluvial ou lacustre - as pioneiras. Via de regra esta vegetação geralmente está associada às áreas inundadas ou brejos próximos aos rios da região. O presente trabalho tem como objetivo construir um mapa da distribuição da vegetação pioneira no Pantanal brasileiro. Utilizaram-se dados levantados pelo projeto Probio-Pantanal, que foram trabalhados e cruzados por meio do programa Spring. A vegetação pioneira se localiza em faixas por todo lado Oeste do Pantanal, e ainda com algumas manchas no nordeste e sudeste, totalizando 5.212 km², ocupando 3,76% da área da planície ou 3,46% quando se considera a área do Bioma. As Formações Pioneiras foram encontradas sobre solos com pouca capacidade de drenagem e próximo aos principais rios pantaneiros. Desta forma, foi possível localizar a vegetação pioneira no Pantanal brasileiro, e quais fatores contribuem para seu aparecimento.Geopantanal 2010

Caracterização da cobertura vegetal e uso da terra na sub-bacia hidrográfica do médio e baixo rio Taquari - MS em 2007.

Resumo: O rio Taquari é um importante afluente do rio Paraguai, fazendo parte, desta forma, da composição do Bioma Pantanal. A bacia do Taquari apresenta em sua área de planalto (sub-bacia do alto Taquari), predomínio de fortes processos erosivos e nas regiões médias e baixas, o transporte e deposição dos sedimentos (sub-bacia do médio e baixo Taquari). Foi caracterizada a cobertura vegetal da sub-bacia do médio e baixo Taquari no Estado de Mato Grosso do Sul em 2007. Utilizaram-se dados já existentes, que foram trabalhados e cruzados por meio do Sistema de Processamento de Informações Georeferenciadas (Spring). As vegetações naturais que apresentam maior ocorrência são a Cerrado (52%) e Chaco (8%), que se encontram em regiões opostas da sub-bacia. Pode-se também concluir que nas áreas desmatadas a maior ocorrência de uso foi a de Pastagem Plantada (6%), não possuindo áreas de Agricultura. Desta forma, foi possível a caracterização da cobertura da sub-bacia do baixo e médio Taquari, estabelecendo parâmetros para próximos estudos e para uso no plano estadual de recursos hídricos do Estado de Mato Grosso do Sul..Geopantanal 2012

Is Gliese 581d habitable? Some constraints from radiative-convective climate modeling

The recently discovered exoplanet Gl581d is extremely close to the outer edge of its system's habitable zone, which has led to much speculation on its possible climate. We have performed a range of simulations to assess whether, given simple combinations of chemically stable greenhouse gases, the planet could sustain liquid water on its surface. For best estimates of the surface gravity, surface albedo and cloud coverage, we find that less than 10 bars of CO2 is sufficient to maintain a global mean temperature above the melting point of water. Furthermore, even with the most conservative choices of these parameters, we calculate temperatures above the water melting point for CO2 partial pressures greater than about 40 bar. However, we note that as Gl581d is probably in a tidally resonant orbit, further simulations in 3D are required to test whether such atmospheric conditions are stable against the collapse of CO2 on the surface.Comment: 9 pages, 11 figures. Accepted for publication in Astronomy & Astrophysic

Study of impurities in spin-Peierls systems including lattice relaxation

The effects of magnetic and non-magnetic impurities in spin-Peierls systems are investigated allowing for lattice relaxation and quantum fluctuations. We show that, in isolated chains, strong bonds form next to impurities, leading to the appearance of magneto-elastic solitons. Generically, these solitonic excitations do not bind to impurities. However, interchain elastic coupling produces an attractive potential at the impurity site which can lead to the formation of bound states. In addition, we predict that small enough chain segments do not carry magnetic moments at the ends

Separation of the magnetic phases at the N\'{e}el point in the diluted spin-Peierls magnet CuGeO3

The impurity induced antiferromagnetic ordering of the doped spin-Peierls magnet Cu(1-x)Mg(x)GeO(3) was studied by ESR technique. Crystals with the Mg concentration x<4% demonstrate a coexistence of paramagnetic and antiferromagnetic ESR modes. This coexistence indicates the separation of a macroscopically uniform sample in the paramagnetic and antiferromagnetic phases. In the presence of the long-range spin-Peierls order (in a sample with x=1.71%) the volume of the antiferromagnetic phase immediately below the N\'{e}el point T_N is much smaller than the volume of the paramagnetic phase. In the presence of the short-range spin-Peierls order (in samples with x=2.88%, x= 3.2%) there are comparable volumes of paramagnetic and antiferromagnetic phases at T=T_N. The fraction of the antiferromagnetic phase increases with lowering temperature. In the absence of the spin-Peierls dimerization (at x=4.57%)the whole sample exhibits the transition into the antiferromagnetic state and there is no phase separation. The phase separation is explained by the consideration of clusters of staggered magnetization located near impurity atoms. In this model the areas occupied by coherently correlated spins expand with decreasing temperature and the percolation of the ordered area through a macroscopic distance occurs.Comment: 7pages, 10 figure

Using the past to constrain the future: how the palaeorecord can improve estimates of global warming

Climate sensitivity is defined as the change in global mean equilibrium temperature after a doubling of atmospheric CO2 concentration and provides a simple measure of global warming. An early estimate of climate sensitivity, 1.5-4.5{\deg}C, has changed little subsequently, including the latest assessment by the Intergovernmental Panel on Climate Change. The persistence of such large uncertainties in this simple measure casts doubt on our understanding of the mechanisms of climate change and our ability to predict the response of the climate system to future perturbations. This has motivated continued attempts to constrain the range with climate data, alone or in conjunction with models. The majority of studies use data from the instrumental period (post-1850) but recent work has made use of information about the large climate changes experienced in the geological past. In this review, we first outline approaches that estimate climate sensitivity using instrumental climate observations and then summarise attempts to use the record of climate change on geological timescales. We examine the limitations of these studies and suggest ways in which the power of the palaeoclimate record could be better used to reduce uncertainties in our predictions of climate sensitivity.Comment: The final, definitive version of this paper has been published in Progress in Physical Geography, 31(5), 2007 by SAGE Publications Ltd, All rights reserved. \c{opyright} 2007 Edwards, Crucifix and Harriso

Dynamic sea level changes following changes in the thermohaline circulation

Using the coupled climate model CLIMBER-3a, we investigate changes in sea surface elevation due to a weakening of the thermohaline circulation (THC). In addition to a global sea level rise due to a warming of the deep sea, this leads to a regional dynamic sea level change which follows quasi-instantaneously any change in the ocean circulation. We show that the magnitude of this dynamic effect can locally reach up to ~1m, depending on the initial THC strength. In some regions the rate of change can be up to 20-25 mm/yr. The emerging patterns are discussed with respect to the oceanic circulation changes. Most prominent is a south-north gradient reflecting the changes in geostrophic surface currents. Our results suggest that an analysis of observed sea level change patterns could be useful for monitoring the THC strength.Comment: Climate Dynamics (2004), submitted. See also http://www.pik-potsdam.de/~ander

Quantal phases, disorder effects and superconductivity in spin-Peierls systems

In view of recent developments in the investigation on cuprate high-T${}_{\rm c}$ superconductors and the spin-Peierls compound CuGeO${}_{3}$, we study the effect of dilute impurity doping on the spin-Peierls state in quasi-one dimensional systems. We identify a common origin for the emergence of antiferromagnetic order upon the introduction of static vacancies, and superconductivity for mobile holes.Comment: 4 pages revtex; revised versio

A quantum isomonodromy equation and its application to N=2 SU(N) gauge theories

We give an explicit differential equation which is expected to determine the instanton partition function in the presence of the full surface operator in N=2 SU(N) gauge theory. The differential equation arises as a quantization of a certain Hamiltonian system of isomonodromy type discovered by Fuji, Suzuki and Tsuda.Comment: 15 pages, v2: typos corrected and references added, v3: discussion, appendix and references adde