Is the coarse-grid Global Climate Model a useful tool for regional paleoclimate reconstruction?

This study considers the climate at the time of the Weichselian ice sheet maximum in Central Europe, especially in Poland, in respect of the NASA Educational version of Global Climate Model (EdGCM). The final results of the EdGCM simulations for the Last Glacial Maximum (LGM) are presented here and these have been analysed to determine whether or not they are useful for regional scale modelling; the problem being that, in a global climate model, both horizontal and vertical grid resolution is very low. Also, an attempt has been made to define the role of the ice megalobe which, in terms of the numerical coarse-grid model,covered the northern parts of Germany and Poland. The broad details of the climate during the Weichselian are defined and our results are compared with previous opinion. The influence of ice megalobe on regional climate is demonstrated and it is also concluded that a coarse-grid global climate model could be a helpful tool in a regional climate recognition. However, whether at a regional or local scale, it is recommended that a specially-configured version of a Regional Climate Model (RCM) based on Global Climate Model (GCM) boundary conditions be used in similar reconstructions

Biblioteki świata w Bibliotece Głównej AGH – współpraca bibliotekarzy BG AGH i stypendystów UNESCO

The author presents a brief description of the category of foreign users of ML AGH UST. She also presents the experience of cooperation of ML AGH UST librarians and scholars of the UNESCO Chair for Science, Technology and Engineering Education programme. Thanks to their cooperation you can get familiarised with the opinions, expectations and ideas of users about the scientific libraryAutorka przedstawia krótką charakterystykę kategorii użytkowników zagranicznych w BG AGH. Prezentuje doświadczenia ze współpracy bibliotekarzy BG AGH i stypendystów programu UNESCO Chair for Science, Technology and Engineering Education, dzięki którym można poznać opinie, oczekiwania i wyobrażenia użytkowników o bibliotece naukowej

Doświadczenia użytkowników Biblioteki Głównej AGH w Krakowie w świetle badań satysfakcji

Autorzy przedstawiają wyniki badań satysfakcji użytkowników Biblioteki Głównej AGH w Krakowie przeprowadzonych w okresie od 27 lutego do 30 kwietnia 2017 r. w ramach projektu Analiza Funkcjonowania Bibliotek Naukowych. Prezentują cele i problemy badawcze, metodykę i narzędzie badawcze oraz analizę wyników wraz z wyborem najważniejszych i najczęstszych komentarzy dodanych przez ankietowanych

Reconstructing dynamics of the Baltic Ice Stream Complex during deglaciation of the Last Scandinavian Ice Sheet

Landforms left behind by the last Scandinavian Ice Sheet (SIS) offer an opportunity to investigate controls governing ice sheet dynamics. Terrestrial sectors of the ice sheet have received considerable attention from landform and stratigraphic investigations. In contrast, despite its geographical importance, the Baltic Sea remains poorly constrained due to limitations in bathymetric data. Both ice-sheet-scale investigations and regional studies at the southern periphery of the SIS have considered the Baltic depression to be a preferential route for ice flux towards the southern ice margin throughout the last glaciation. During the deglaciation the Baltic depression hosted the extensive Baltic Ice Lake, which likely exerted a considerable control on ice dynamics. Here we investigate the Baltic depression using newly available bathymetric data and peripheral topographic data. These data reveal an extensive landform suite stretching from Denmark in the west to Estonia in the east and from the southern European coast to the Åland Sea, comprising an area of 0.3 million km2. We use these landforms to reconstruct aspects of the ice dynamic history of the Baltic sector of the ice sheet. Landform evidence indicates a complex retreat pattern that changes from lobate ice margins with splaying lineations to parallel mega-scale glacial lineations (MSGLs) in the deeper depressions of the Baltic Basin. Ice margin still-stands on underlying geological structures indicate the likely importance of pinning points during deglaciation, resulting in a stepped retreat signal. Over the span of the study area we identify broad changes in the ice flow direction, ranging from SE–NW to N–S and then to NW–SE. MSGLs reveal distinct corridors of fast ice flow (ice streams) with widths of 30 km and up to 95 km in places, rather than the often-interpreted Baltic-wide (300 km) accelerated ice flow zone. These smaller ice streams are interpreted as having operated close behind the ice margin during late stages of deglaciation. Where previous ice-sheet-scale investigations inferred a single ice source, our mapping identifies flow and ice margin geometries from both Swedish and northern Bothnian sources. We anticipate that our landform mapping and interpretations may be used as a framework for more detailed empirical studies by identifying targets to acquire high-resolution bathymetry and sediment cores and also for comparison with numerical ice sheet modelling.</p

GIS dataset: geomorphological record of terrestrial-terminating ice streams, southern sector of the Baltic Ice Stream Complex, last Scandinavian Ice Sheet, Poland

Here we present a comprehensive dataset of glacial geomorphological features covering an area of 65 000 km2 in central west Poland, located along the southern sector of the last Scandinavian Ice Sheet, within the limits of the Baltic Ice Stream Complex. The GIS dataset is based on mapping from a 0.4 m high-resolution digital elevation model derived from airborne light detection and ranging data. Ten landform types have been mapped: mega-scale glacial lineations, drumlins, marginal features (moraine chains, abrupt margins, edges of ice-contact fans), ribbed moraines, tunnel valleys, eskers, geometrical ridge networks, and hill–hole pairs. The map comprises 5461 individual landforms or landform parts, which are available as vector layers in GeoPackage format at https://doi.org/10.5281/zenodo.4570570 (Szuman et al., 2021a). These features constitute a valuable data source for reconstructing and modelling the last Scandinavian Ice Sheet extent and dynamics from the Middle Weichselian Scandinavian Ice Sheet advance, 50–30 ka, through the Last Glacial Maximum, 25–21 ka, and Young Baltic advances, 18–15 ka. The presented data are particularly useful for modellers, geomorphologists, and glaciologists

The anti-proliferative and anti-bacterial activity of argan oil and crude saponin extract from Argania spinosa (L.) skeels

INTRODUCTION: Argan oil is a well-known cosmeceutical that is commercially available. It is traditionally used for the treatment of acne and skin inflammation among others. The objective of this study was to assess the anti-proliferative and antibacterial activities of argan oil and a crude saponin extract from the argan tree (Argania spinosa (L.) Skeels) that is endemic to Morocco. MATERIALS AND METHODS: The anti-proliferative activity of argan oil and the crude saponin extract was assessed by the 2,3-bis-(2-methoxy-4-nitro-5-sulfophenyl)-2H-tetrazolium-5-carboxanilide (XTT) assay on A431; HaCat; HeLa; MCF-7 and UCT-Mel 1 cells. The antibacterial activity was evaluated by the broth microdilution method against two species of bacteria: Cutibacterium acnes and Prevotella intermedia. RESULTS: The results of this study indicated that the argan oil sample did not inhibit the cell growth of the specified cell lines up to 1000µg/ml, while the crude saponin extract had low anti-proliferative activity. The minimal inhibitory concentration (MIC) values for both the argan oil and the crude saponin extract were found to be 500µg/ml against Cutibacterium acnes. No antibacterial activity from the argan oil or the crude saponin extract was evident against Prevotella intermedia up to a concentration of 12.5mg/ml. CONCLUSION: The results of this study indicated that argan oil and the crude saponin extract might have direct inhibitory effects on the growth and proliferation of Cutibacterium acnes. This finding supports the use argan oil as a treatment for acne vulgaris.National Research Foundationhttp://www.phcogfirst.com/content/pharmacognosy-journalpm2020Plant Production and Soil Scienc

Three-dimensional numerical model of heat losses from district heating network pre-insulated pipes buried in the ground

The purpose of the paper is to investigate the challenges in modelling the energy losses of heating networks and to analyse the factors that influence them. The verification of the simulation was conducted on a test stand in-situ and based on the measurements of the testing station, a database for the final version of the numerical model was developed and a series of simulations were performed. Examples of the calculated results are shown in the graphs. The paper presents an innovative method of identify the energy losses of underground heating network pipelines and quantify the temperature distribution around them, in transient working conditions. The presented method makes use of numerical models and measured data of actual objects.The dimensions of the pipelines used were 6m wide, 8m high and 1m in depth, while they were simulated under conditions of zero heat flow in the ground, in the perpendicular to the sides direction of the calculated area and considering the effects of ground's thermal conductivity. The mesh was developed using advanced functions, which resulted its high quality with the average orthogonal quality of 0.99 (close to 1.00) and Skewness of 0.05 (between 0.00 and 0.25). To achieve better accuracy of the simulation model, the initial conditions were determined based on the numerical results of a three-dimensional analysis of heat losses, in steady state conditions in a single moment. The validation process confirmed the high quality of the model, as the differences between the ground temperatures were approximately 0.1°C

Why is IPv6 Deployment Important for the Internet Evolution?, Journal of Telecommunications and Information Technology, 2011, nr 2

Replacing the IPv4 protocol with IPv6 on the Internet is currently one of the aims of the European Union policy. The main reason for this replacement is the effeteness of the addresses pool in the IPv4 protocol, which can cause serious complications in the evolution of the Internet and its adaptation in new areas, e.g., in next generation mobile telephony or the so called Internet of Things. Simultaneously, the addressing capabilities of the IPv6 protocol are practically unlimited and its new functionalities increase the attractiveness of its usage. The article discusses the problems connected with the IPv6 deployment on the Internet. Especially, the rules for realization of the IPv6 deployment and rules for cooperation of IPv4 with IPv6 (including cooperation tests) in network infrastructure and in applications are presented. Moreover, the European projects’ results and the activity’s directions of the national project Future Internet Engineering are discussed