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The impact of hazardous waste on people and the environment from agricultural, industrial, military and mining activities form one of the most significant global environmental challenges. These wastes often include heavy metals, acid precipitates (sulfur oxide solutions), hydrocarbons, and other organic chemicals. Environmental impact of such technogenic waste and dumps sources (TWDS) is widely reflected in vegetation cover changes, which can be easily detected by satellite instruments. But application of satellite data for TWDS monitoring requires appropriate information tools. At presented work, the authors conducted the development of the design and implementation of these tools within frames VEGA-Science services (http://sci-vega.ru/eng/) in order to provide analysis of longterm variability of the vegetation cover state caused by the influence of TWDS. The result of the work was included in automated system for remote monitoring of vegetation cover (SRMV) of VEGA-Science system.

Satellite radiothermovision is a set of processing techniques applicable for multisource data of radiothermal monitoring of oceanatmosphere system, which allows creating dynamic description of mesoscale and synoptic atmospheric processes and estimating physically meaningful integral characteristics of the observed processes (like avdective flow of the latent heat through a given border). The approach is based on spatiotemporal interpolation of the satellite measurements which allows reconstructing the radiothermal fields (as well as the fields of geophysical parameters) of the ocean-atmosphere system at global scale with spatial resolution of about 0.125° and temporal resolution of 1.5 hour. The accuracy of spatiotemporal interpolation was estimated by direct comparison of interpolated data with the data of independent asynchronous measurements and was shown to correspond to the best achievable as reported in literature (for total precipitable water fields the accuracy is about 0.8 mm). The advantages of the implemented interpolation scheme are: closure under input radiothermal data, homogeneity in time scale (all data are interpolated through the same time intervals), automatic estimation of both the intermediate states of scalar field of the studied geophysical parameter and of vector field of effective velocity of advection (horizontal movements). Using this pair of fields one can calculate the flow of a given geophysical quantity though any given border. For example, in case of total precipitable water field, this flow (under proper calibration) has the meaning of latent heat advective flux. This opportunity was used to evaluate the latent heat flux though a set of circular contours, enclosing a tropical cyclone and drifting with it during its evolution. A remarkable interrelation was observed between the calculated magnitude and sign of advective latent flux and the intensity of a tropical cyclone. This interrelation is demonstrated in several examples of hurricanes and tropical cyclones of August, 2000, and typhoons of November, 2013, including super typhoon Haiyan.

Numerous applications of Earth observation (EO) data for Earth resource exploration both for land use management purposes and for fundamental research goals require as much as possible independent EO data sets provided for a number of data consumers, i.e. for collective (shared) data usage. In addition data distribution procedures should be accompanied with sophisticated information services enabling correct interpretation and application of provided data. As a result data providers should be able to convert data in a lot of consumer-proper formats and in some cases it should require additional data processing before data shipping. Presented work proposes basic infrastructure for collective (shared) EO data usage that enables above mentioned integration of information resources contained in typical Russian EO centers. Paper reveals architecture design, description of basic infrastructure elements, and examples of real implementations.

This literature review focuses on the use of corifollitropin alfa for ovarian stimulation in assisted reproductive technology (ART) programmes in different groups of patients. Corifollitropin alfa is a gonadotropin drug with prolonged FSH activity. The main difference between corifollitropin alfa and other gonadotropins is the higher level of peak FSH, which leads to the recruitment of more follicles. Another feature is the inability to adjust the gonadotropin dose during the first days of ovarian stimulation. In contrast to traditional indications/contraindications for gonadotropins, the use of cortifollitropin is not recommended in combination with GnRH agonists or in patients with polycystic ovary syndrome.Evidence for the feasibility and efficacy of using corifollitropin alfa in patients with various ovarian response variants in ART programmes has been analysed. Most researchers agree that the use of corifollitropin alfa can be recommended for patients with a presumed poor or normal ovarian response. The use of corifollitropin alfa in patients with a presumed excessive response to ovarian timulation is possible when embryo transfer is not expected: in oocyte donation/oocyte vitrification cycles or in "freeze-all" cycles.A significant advantage of using corifollitropin alfa for oocyte donor patients is the single administration of the drug, which can be done in a medical facility, which reduces the risk of prescription non-compliance.The use of corifollitropin alfa in protocols with GnRH agonists requires further research: firstly, corifollitropin alfa has no LH component and secondly, there is no possibility of ovulation trigger replacement in this protocol if there is a high risk of early ovarian hyperstimulation syndrome.