The role of civil affairs in unconventional warfare

With the renewed focus on Unconventional Warfare as a means of achieving U.S. Foreign and National Security Policy goals, the U.S. Army Special Operations Command Civil Affairs force must assess its capability to conduct Civil Affairs operations in support of an Unconventional Warfare campaign. This thesis examines Civil Affairs current role and surveys past conflicts to explore Civil Affairs potential role in all phases of Unconventional Warfare. It assumes that political and logistical networks are the keys to building and sustaining a revolutionary movement. This thesis answers the following questions How can Civil Affairs forces in place now and deployed for an operation identify, develop and motivate revolutionary networks that can be activated to sustain a revolution and fulfill U.S. policy needs within a foreign nation How can Civil Affairs doctrine be revised to better support these taskshttp://archive.org/details/theroleofcivilff1094527789Master Sergeant, United States ArmyMajor, United States ArmyApproved for public release; distribution is unlimited

Notostraca trackways in Permian playa environments of the Lodève basin (France)

Durante casi veinte años, el Dr Lapeyrie, cirujano en Lodève, ha reunido numerosos fósiles provenientes de la Formación del Salagou de la cuenca pérmica de Lodève. Los mismos incluyen insectos, notostráceos, plantas e icnofósiles. Entre los últimos, hay una multitud de pistas de artrópodos, muy bien preservadas, las cuales fueron recogidas en el techo de secuencias depositadas en alrededores de lagos tipo playa. Experimentos sobre locomoción de artrópodos efectuados con animales actuales sugieren que la mayoría de las pistas estudidas fueron producidas por Notostracos de los cuales se han encontrado algunos millares de restos (caparazónes, apéndices, cuerpos enteros) asignados a Triops cancriformis permiensis y Lepidurus occitaniacus. Todos estos rastros fueron producidos de forma subacuática y corresponden a diferentes eto-morfotipos conocidos en la literatura con el nombre de Acripes para las huellas de locomoción, de Rusophycus para las de descanso y excavación (posiciones horizontales, proclinales y opistoclinales) y de Cruziana para locomoción y excavación activa. Numerosas planchas fósiliferas permiten ver claramente el paso de una actividad a la otra. Esta situación fue registrada en una película con Lepidurus actuales. Se reconocieron los icnotaxones Acribes multiformis nov. isp, Rusophycus eutendorfensis, R. carbonarius, R. versans, R. minutus, R. furcosus, Cruziana problematica, C. pascens y, menos abundantemente, Scoyenia isp. También fueron encontradas numerosas pisadas, destacando la icnofacies Scoyenia, encontrándose solamente en los «overbank settings». Para la Formación del Salagou, éstos corresponden a llanuras de inundación/playas donde las zonas inundadas eran temporales y de poca profundidad, y en las que vivían Notostracos, Insectos, Aracnidos y Concostracos (= Spinicaudata + Laevicaudata), este último grupo conocido solamente por cuerpos-fósiles. Este ambiente de playa distal, desarrollado en un clima árido, ha perdurado durante una gran parte del Pérmico, posiblemente entre el Cisuraliense superior y el Lopingiense inferior

Fluoxetine effects assessment on the life cycle of aquatic invertebrates

International audienceFluoxetine is a serotonin re-uptake inhibitor, generally used as an antidepressant. It is suspected to provoke substantial effects in the aquatic environment. This study reports the effects of fluoxetine on the life cycle of four invertebrate species, Daphnia magna, Hyalella azteca and the snail Potamopyrgus antipodarum exposed to fluoxetine spiked-water and the midge Chironomus riparius exposed to fluoxetine-spiked sediments. For D. magna, a multi-generational study was performed with exposition of newborns from exposed organisms. Effects of fluoxetine could be found at low measured concentrations (around 10 micro g l(-1)), especially for parthenogenetic reproduction of D. magna and P. antipodarum. For daphnids, newborns length was impacted by fluoxetine and the second generation of exposed individuals showed much more pronounced effects than the first one, with a NOEC of 8.9 micro g l(-1). For P. antipodarum, significant decrease of reproduction was found for concentrations around 10 micro g l(-1). In contrast, we found no effect on the reproduction of H. azteca but a significant effect on growth, which resulted in a NOEC of 33 micro g l(-1), expressed in nominal concentration. No effect on C. riparius could be found for measured concentrations up to 59.5 mg kg(-1). General mechanistic energy-based models showed poor relevance for data analysis, which suggests that fluoxetine targets specific mechanisms of reproduction

Nanofiltration of lactic acid whey: A process to improve the dryability and the quality of powder

Nanofiltration of lactic acid whey: A process to improve the dryability and the quality of powder. 6. European Drying Conference: EuroDrying 201

Measuring global mean sea level changes with surface drifting buoys

Combining ocean model data and in-situ Lagrangian data, I show that an array of surface drifting buoys tracked by a Global Navigation Satellite System (GNSS), such as the Global Drifter Program, could provide estimates of global mean sea level (GMSL) and its changes, including linear decadal trends. For a sustained array of 1250 globally distributed buoys with a standardized design, I demonstrate that GMSL decadal linear trend estimates with an uncertainty less than 0.3 mm yr$^{-1}$ could be achieved with GNSS daily random error of 1.6 m or less in the vertical direction. This demonstration assumes that controlled vertical position measurements could be acquired from drifting buoys, which is yet to be demonstrated. Development and implementation of such measurements could ultimately provide an independent and resilient observational system to infer natural and anthropogenic sea level changes, augmenting the on-going tide gauge and satellites records.Comment: resubmitted to AGU Geophysical Research Letter

Contribution of future wide-swath altimetry missions to ocean analysis and forecasting

The impact of forthcoming wide-swath altimetry missions on the ocean analysis and forecasting system was investigated by means of OSSEs (observing system simulation experiments). These experiments were performed with a regional data assimilation system, implemented in the Iberian–Biscay–Ireland (IBI) region, at 1∕12° resolution using simulated observations derived from a fully eddy-resolving free simulation at 1∕36° resolution over the same region. The objective of the experiments was to assess the ability of different satellite constellations to constrain the ocean analyses and forecasts, considering both along-track altimeters and future wide-swath missions; consequently, the capability of the data assimilation techniques used in the Mercator Ocean operational system to effectively combine the different kinds of measurements was also investigated. These assessments were carried out as part of a European Space Agency (ESA) study on the potential role of wide-swath altimetry in future versions of the European Union Copernicus programme. The impact of future wide-swath altimetry data is evident for investigating the reliability of sea level values in OSSEs. The most significant results were obtained when looking at the sensitivity of the system to wide-swath instrumental error: considering a constellation of three nadir and two accurate (small instrumental error) wide-swath altimeters, the error in ocean analysis was reduced by up to 50&thinsp;% compared to conventional altimeters. Investigating the impact of the repetitivity of the future measurements, the results showed that two wide-swath missions had a major impact on sea-level forecasting – increasing the accuracy over the entire time window of the 5-day forecasts – compared with a single wide-swath instrument. A spectral analysis underlined that the contributions of wide-swath altimetry data observed in ocean analyses and forecast statistics were mainly due to the more accurate resolution, compared with along-track data, of ocean variability at spatial scales smaller than 100&thinsp;km. Considering the ocean currents, the results confirmed that the information provided by wide-swath measurements at the surface is propagated down the water column and has a considerable impact (30&thinsp;%) on ocean currents (up to a depth of 300&thinsp;m), compared with the present constellation of altimeters. The ocean analysis and forecasting systems used here are those currently used by the Copernicus Marine Environment and Monitoring Service (CMEMS) to provide operational services and ocean reanalysis. The results obtained in the OSSEs considering along-track altimeters were consistent with those derived from real data (observing system experiments, OSEs). OSSEs can also be used to assess the potential of new observing systems, and in this study the results showed that future constellations of altimeters will have a major impact on constraining the CMEMS ocean analysis and forecasting systems and their applications.</p

Eddy-Permitting Ocean Circulation Hindcasts of Past Decades

International audienc

Oceanic hindcast simulations at high resolution suggest that the Atlantic MOC is bistable

All climate models predict a freshening of the North Atlantic at high latitude that may induce an abrupt change of the Atlantic Meridional Overturning Circulation (hereafter AMOC) if it resides in the bistable regime, where both a strong and a weak state coexist. The latter remains uncertain as there is no consensus among observations and ocean reanalyses, where the AMOC is bistable, versus most climate models that reproduce a mono-stable strong AMOC. A series of four hindcast simulations of the global ocean at 1/12° resolution, which is presently unique, are used to diagnose freshwater transport by the AMOC in the South Atlantic, an indicator of AMOC bistability. In all simulations, the AMOC resides in the bistable regime: it exports freshwater southward in the South Atlantic, implying a positive salt advection feedback that would act to amplify a decreasing trend in subarctic deep water formation as projected in climate scenarios