Ice mass change in Greenland and Antarctica between 1993 and 2013 from satellite gravity measurements     

Matthieu J. Talpe  R. Steven Nerem  Ehsan Forootan  Michael Schmidt  Frank G. Lemoine  Ellyn M. Enderlin  Felix W. Landerer 《Journal of Geodesy》2017,91(11):1283-1298

We construct long-term time series of Greenland and Antarctic ice sheet mass change from satellite gravity measurements. A statistical reconstruction approach is developed based on a principal component analysis (PCA) to combine high-resolution spatial modes from the Gravity Recovery and Climate Experiment (GRACE) mission with the gravity information from conventional satellite tracking data. Uncertainties of this reconstruction are rigorously assessed; they include temporal limitations for short GRACE measurements, spatial limitations for the low-resolution conventional tracking data measurements, and limitations of the estimated statistical relationships between low- and high-degree potential coefficients reflected in the PCA modes. Trends of mass variations in Greenland and Antarctica are assessed against a number of previous studies. The resulting time series for Greenland show a higher rate of mass loss than other methods before 2000, while the Antarctic ice sheet appears heavily influenced by interannual variations.  相似文献   

“There is No Program Without Farmers”: Interactive Radio for Forest Landscape Restoration in Mount Elgon Region,Uganda     

Karen Hampson  Mark Leclair  Askebir Gebru  Lynne Nakabugo  Chris Huggins 《社会与自然资源》2017,30(5):642-657

Increase in ownership and use of radios and mobile phones in Uganda may present opportunities for interactive and efficient agricultural extension services. Yet the impact of interactive radio on rural development has rarely been evaluated. In a participatory project, the International Union for the Conservation of Nature together with Farm Radio International and stakeholders from local government, radio, and community-based organizations promoted the increased use of forest landscape restoration activities though interactive rural radio programs, including innovative methods to reach populations not covered by radio. An evaluation found that 98% of people who listened to most or all of the broadcasts carried out one of the practices, whereas 84% of those who had listened to only one episode had used one of the practices. Inclusion of a wide range of community stakeholders from project inception was vital for presenting the project and embedding it within local institutional contexts.  相似文献   

The Rwenzori Mountains,a landslide-prone region?     

Liesbet Jacobs  Olivier Dewitte  Jean Poesen  Damien Delvaux  Wim Thiery  Matthieu Kervyn 《Landslides》2016,13(3):519-536

With its exceptionally steep topography, wet climate, and active faulting, landslides can be expected to occur in the Rwenzori Mountains. Whether or not this region is prone to landsliding and more generally whether global landslide inventories and hazard assessments are accurate in data-poor regions such as the East African highlands are thus far unclear. In order to address these questions, a first landslide inventory based on archive information is built for the Rwenzori Mountains. In total, 48 landslide and flash flood events, or combinations of these, are found. They caused 56 fatalities and considerable damage to road infrastructure, buildings, and cropland, and rendered over 14,000 persons homeless. These numbers indicate that the Rwenzori Mountains are landslide-prone and that the impact of these events is significant. Although not based on field investigations but on archive data from media reports and laymen accounts, our approach provides a useful complement to global inventories overlooking this region and increases our understanding of the phenomenon in the Rwenzori Mountains. Considering the severe impacts of landslides, the population growth and related anthropogenic interventions, and the likelihood of more intense rainfall conditions, there is an urgent need to invest in research on disaster risk reduction strategies in this region and other similar highland areas of Africa.  相似文献   

Reconstruction of a flash flood event through a multi-hazard approach: focus on the Rwenzori Mountains,Uganda     

Liesbet Jacobs  Jan Maes  Kewan Mertens  John Sekajugo  Wim Thiery  Nicole van Lipzig  Jean Poesen  Matthieu Kervyn  Olivier Dewitte 《Natural Hazards》2016,84(2):851-876

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Liquid water uptake in unconfined Callovo Oxfordian clay-rock studied with neutron and X-ray imaging     

Stavropoulou  Eleni  Andò  Edward  Tengattini  Alessandro  Briffaut  Matthieu  Dufour  Frédéric  Atkins  Duncan  Armand  Gilles 《Acta Geotechnica》2019,14(1):19-33

The Callovo Oxfordian clay-rock (COx) is studied in France for the disposal of radioactive waste, because of its extremely low permeability. This host rock is governed by a hydromechanical coupling of high complexity. This paper presents an experimental study into the mechanisms of water uptake in small, unconfined, prismatic specimens of COx, motivated by the comprehension of cracking observed during concrete/COx interface sample preparation. Water uptake is monitored using both X-ray tomography and neutron radiography, the combination of these imaging techniques allowing material deformation and water arrival to be quantified, respectively. Given the speed of water entry and crack propagation, relatively fast imaging is required: 5-min X-ray tomographies and 10-s neutron radiographs are used. In this study, pairs of similar COx samples from the same core are tested separately with each imaging technique. Two different orientations with respect to the core are also investigated. Analysis of the resulting images yields with micro- and macro-scale insights into hydromechanical mechanisms to be obtained. This allows the cracking to be interpreted as a rapid breakdown in capillary suction (supposed large both to drying and rebound from in situ stress state) due to water arrival, which in turn causes a loss of effective stress, allowing cracks to propagate and deliver water further into the material.

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Holocene phreatomagmatic eruptions alongside the densely populated northern shoreline of Lake Kivu,East African Rift: timing and hazard implications     

Sam Poppe  Benoît Smets  Karen Fontijn  Montfort Bagalwa Rukeza  Antoine De Marie Fikiri Migabo  Albert Kyambikwa Milungu  Didier Birimwiragi Namogo  François Kervyn  Matthieu Kervyn 《Bulletin of Volcanology》2016,78(11):82

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Objective assessment of the contribution of the RECOPESCA network to the monitoring of 3D coastal ocean variables in the Bay of Biscay and the English Channel     

Julien Lamouroux  Guillaume Charria  Pierre De Mey  Stéphane Raynaud  Catherine Heyraud  Philippe Craneguy  Franck Dumas  Matthieu Le Hénaff 《Ocean Dynamics》2016,66(4):567-588

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First-arrival traveltime tomography using second generation wavelets     

Matthieu Delost  Jean Virieux  Stéphane Operto 《Geophysical Prospecting》2008,56(4):505-526

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Preservation of cross-sets due to migration of current ripples over aggrading and non-aggrading beds: comparison of experimental data with theory   总被引：1，自引：0，他引：1  

Joep E. A. Storms  Remke L. Van Dam  & Suzanne F. Leclair 《Sedimentology》1999,46(1):189-200

An experimental study of the preservation of cross-sets during the migration of current ripples under aggrading and non-aggrading conditions was conducted in order to test the modified Paola–Borgman theory for distribution of cross-set thickness as a function of distribution of bed-wave height. In a series of flume experiments, the geometry and migration characteristics of the ripples did not vary systematically with aggradation rate and are comparable to other flume and river data.
Mean cross-set thickness/mean formative bed-wave height is less than 0·4, and mean cross-set thickness/mean bed-wave height is less than 0·53. In the present experiments, the primary control of cross-set thickness is the variability of ripple height. Aggradation rate accounts for only 1–7% of the total cross-set thickness.
A two-parameter gamma density function was fitted to histograms of ripple height to determine the value of parameter a needed for the modified Paola–Borgman model. This model underestimates cross-set thickness because of its assumption that bed-form height spreads evenly above and below the mean bed level, which is not the case in reality. Mean cross-set thickness is predicted quite well if the model constant is increased to 1·3.  相似文献   

Tropical drought patterns and their linkages to large-scale climate variability over Peninsular Malaysia     

Qing He  Kwok Pan Chun  Mou Leong Tan  Bastien Dieppois  Liew Juneng  Julian Klaus  Matthieu Fournier  Nicolas Massei  Omer Yetemen 《水文研究》2021,35(9):e14356

Ocean–atmosphere modes of climate variability in the Pacific and Indian oceans, as well as monsoons, regulate the regional wet and dry episodes in tropical regions. However, how those modes of climate variability, and their interactions, lead to spatial differences in drought patterns over tropical Asia at seasonal to interannual time scales remains unclear. This study aims to analyse the hydroclimate processes for both short- and long-term spatial drought patterns (3-, 6, 12- and 24-months) over Peninsular Malaysia using the Standardized Precipitation Index, Standardized Precipitation Evapotranspiration Index, and Palmer Drought Severity Index. Besides that, a generalized least squares regression is used to explore underlying circulation mechanisms of these spatio-temporal drought patterns. The tested drought indices indicate a tendency towards wetter conditions over Peninsular Malaysia. Based on principal component analysis, distinct spatio-temporal drought patterns are revealed, suggesting North–South and East–West gradients in drought distribution. The Pacific El Nino Southern Oscillation (ENSO), the South Western Indian Ocean (SWIO) variability, and the quasi-biennial oscillation (QBO) are significant contributors to the observed spatio-temporal variability in drought. Both the ENSO and the SWIO modulate the North–South gradient in drought conditions over Peninsular Malaysia, while the QBO contributes more to the East–West gradient. Through modulating regional moisture fluxes, the warm phases of the ENSO and the SWIO, and the western phases of the QBO weaken the southwest and northeast monsoon, leading to precipitation deficits and droughts over Peninsular Malaysia. The East–West or North–South gradients in droughts are related to the middle mountains blocking southwest and northeast moisture fluxes towards Peninsular Malaysia. In addition, the ENSO and QBO variations are significantly leading to short-term droughts (less than a year), while the SWIO is significantly associated with longer-duration droughts (2 years or more). Overall, this work demonstrates how spatio-temporal drought patterns in tropical regions are related to monsoons and moisture transports affected by the oscillations over the Pacific and Indian oceans, which is important for national water risk management.  相似文献