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241.
242.
Niels Rodskjer 《Theoretical and Applied Climatology》1964,13(2):261-269
Summary It is shown that the current of a pyranometer can be made independent of temperature by connecting a resistor of appropriate characteristics in series with the pyranometer. The temperature coefficient of the pyranometer with respect to the electromotive force should be made equal to the temperature coefficient of the resistance of the circuit. A resistor with a semilinear temperature characteristic and a negative temperature coefficient can be constructed by connecting a N.T.C. (Negative Temperature Coefficient) resistor in parallel with a resistor of constant resistance. A complete calculation is carried out for a case where the pyranometer is a Moll-Gorczynski solarimeter and the instrument indicating the current is a potentiometer. It turns out that the temperature influence on the radiation measurement can be almost eliminated.
With 4 Figures 相似文献
Zusammenfassung Es wird gezeigt, daß der Strom eines Pyranometers durch Einbau eines Resistors von geeigneter Charakteristik in Serie mit dem Pyranometer temperaturunabhängig gemacht werden kann. Zu diesem Zweck ist der Temperaturkoeffizient des Pyranometers in bezug auf die elektromotorische Kraft dem Temperaturkoeffizienten des Widerstandes des Stromkreises gleich zu machen. Ein Resistor mit einer semilinearen Temperaturcharakteristik und einem negativen Temperaturkoeffizienten kann durch Verbindung eines resistors mit negativen Temperaturkoeffizienten (N. T. C.) parallel zu einem Resistor von konstantem Widerstand konstruiert werden. Es wird eine vollständige Berechnung für den Fall der Kombination eines Solarimeters Moll-Gorczynski mit einem Potentiometer durchgeführt. Dabei ergibt sich, daß der Temperatureinfluß auf die Strahlungsmessung nahezu eliminiert werden kann.
Résumé L'auteur démontre que le courant issu d'une pyranomètre peut être rendu indépendant des influences de la température en introduisant dans le circuit une thermistance appropriée placée en série. Le coefficient thermique du pyranomètre—compte tenu de la force électromotrice—doit être égal au coefficient thermique de la résistance du circuit. On peut construire une thermistance avec une caractéristique semi-linéaire de température et un coefficient thermique négatif en connectant en parallèle une résistance N. T. C. (Negative Temperature Coefficient) et une résistance constante. L'auteur présente un calcul complet pour le cas où le pyranomètre est un solarimètre Moll-Gorczynski et l'instrument de mesure un potentiomètre. Il en résulte que l'influence de la tempature sur la mesure du rayonnement peut presque être éliminée.
With 4 Figures 相似文献
243.
This paper presents sedimentary evidence for rapid englacial debris entrainment during jökulhlaups. Previous studies of jökulhlaup sedimentology have focused predominantly on proglacial impact, rather than depositional processes within glaciers. However, observations of supraglacial floodwater outbursts suggest that englacial sediment emplacement is possible during jökulhlaups. The November 1996 jökulhlaup from Skei?arárjökull, Iceland presented one of the first opportunities to examine englacial flood deposits in relation to former supraglacial outlets. Using observations from Skei?arárjökull, this paper identifies and explains controls on the deposition of englacial flood sediments and presents a qualitative model for englacial jökulhlaup deposition. Englacial jökulhlaup deposits were contained within complex networks of upglacier‐dipping fractures. Simultaneous englacial deposition of fines and boulder‐sized sediment demonstrates that englacial fracture discharge had a high transport capacity. Fracture geometry was an important control on the architecture of englacial jökulhlaup deposits. The occurrence of pervasively frozen flood deposits within Skei?arárjökull is attributed to freeze‐on by glaciohydraulic supercooling. Floodwater, flowing subglacially or through upglacier‐dipping fractures, would have supercooled as it was raised to the surface faster than its pressure‐melting point could increase as glaciostatic pressure decreased. Evidence for floodwater contact with the glacier bed is supported by the ubiquitous occurrence of sheared diamict rip‐ups and intra‐clasts of basal ice within jökulhlaup fractures, deposited englacially some 200–350 m above the bed of Skei?arárjökull. Evidence for fluidal supercooled sediment accretion is apparent within stratified sands, deposited englacially at exceptionally high angles of rest in the absence of post‐depositional disturbance. Such primary sediment structures cannot be explained unless sediment is progressively accreted to opposing fracture walls. Ice retreat from areas of former supraglacial outbursts revealed distinct ridges characterized by localized upwellings of sediment‐rich floodwater. These deposits are an important addition to current models of englacial sedimentation and demonstrate the potential for post‐jökulhlaup landform development. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
244.
René Hudec Pavel Spurný Jan Florián Jaroslav Boček Miloš Tichý Jana Tichá Libor Vyskočil Wolfgang Wenzel Scott Barthelmy Thomas Cline Niels Gehrels Gerald Fishman Chryssa Kouveliotou Charles Meegan Asen Mutafov 《Experimental Astronomy》1997,7(4):319-323
We present first preliminary results obtained with the European Observation Network consisting of 9 observatories in the Czech Republic, Germany and Bulgaria. We also discuss related problems such as the background of unknown variable stars and suggest a strategy for work in this area. 相似文献
245.
246.
Ramster John; Daan Niels; Frid Chris; Megrey Bernard; Payne Andrew; Pepin Pierre 《ICES Journal of Marine Science》2003,60(6):1169-1171
Article 1 of the ICES Convention of 1964 sets out the fundamentalpurposes of the Council and includes as the third and finalpoint: "to publish or otherwise disseminate the results of researchand investigations carried out under its auspices or to encouragethe publication thereof". Publication and dissemination of informationabout the living resources and their environment have been atthe heart of ICES from the first 相似文献
247.
Simple models, analytical and numerical, of plasma temperatures in the Venusian ionosphere are developed. They are applied to thermal-structure data obtained by the Pioneer Venus Orbiter to estimate the magnitudes of important plasma thermal parameters. 相似文献
248.
Charlotte B. Hasager Niels W. Nielsen Niels Otto Jensen Eva Boegh Jens H. Christensen Ebba Dellwik Henrik Soegaard 《Boundary-Layer Meteorology》2003,109(3):227-254
In numerical weather prediction, climate and hydrologicalmodelling, the grid cell size is typically larger than the horizontal length scales of variations in aerodynamicroughness, surface temperature and surface humidity. These local land cover variations give rise to sub-gridscale surface flux differences. Especially the roughness variations can give a significantly differentvalue between the equilibrium roughness in each of the patches as compared to the aggregated roughness value,the so-called effective roughness, for the grid cell. The effective roughness is a quantity that secures thephysics to be well-described in any large-scale model. A method of aggregating the roughness step changesin arbitrary real terrain has been applied in flat terrain (Denmark) where sub-grid scale vegetation-drivenroughness variations are a dominant characteristic of the landscape. The aggregation model is a physicaltwo-dimensional atmospheric flow model in the horizontal domain based on a linearized version of theNavier Stoke equation. The equations are solved by the Fast Fourier Transformation technique, hence the codeis very fast. The new effective roughness maps have been used in the HIgh Resolution Limited Area Model(HIRLAM) weather forecasting model and the weather prediction results are compared for a number of casesto synoptic and other observations with improved agreement above the predictions based on currentstandard input. Typical seasonal springtime bias on forecasted winds over land of +0.5 m s-1 and-0.2 m s-1 in coastal areas is reduced by use of the effective roughness maps. 相似文献
249.
The mass distribution and sorting of tephra produced in the plinian phase of the 1970 Hekla eruption was controlled by the particle size distribution, the height of the eruption column, and velocity of transport. Near the volcano the mass distribution of soluble fluorine was controlled by particle size of the deposits, but approaches the mass distribution of the tephra at longer distances. Adsorbed soluble fluorine reaches a maximum at a distance from the volcano determined by the velocity of the transporting medium.SEM studies show the soluble fluorine to be chemically adsorbed on the surface of tephra particles. The adsorption is shown by experiment to occur at temperatures below 600°C in the cooling eruption column. Evaluation of reactions in the eruption column leads to the conclusion that formation of water soluble compounds adhering to tephra is principally controlled by environmental factors and to a lesser degree by the composition of the volcanic gas phase. 相似文献
250.
This study aims to investigate and model driving forces that lead to increased fishing pressure and an altered state of the environment in the coastal areas near Samsun on the Turkish Black Sea coast. We have applied a modified DPSIR model to structure our investigation and analysis and have investigated the drivers that generate fishing pressure in the Samsun fisheries. The overall health of the ecosystem is declining, and there is a consistent trend of deterioration in the condition of the three major species targeted by the trawl fisheries. Although introduced invasive species have brought significant changes to the Black Sea, it is clear that the state of the environment is significantly and negatively affected by the pressure exerted by fisheries. Fishing pressure has to a certain extent been redirected to pelagic trawling as bottom trawling has become less profitable and a rise in catch capacity has levelled off. This reduction is, however, offset by an increase in illegal trawling and dredging by a very rapidly growing sector of multi-purpose small boats, resulting in a considerable increase in the overall accumulated engine power of fishing boats in Samsun during 2000–2005. Fisheries in Samsun, in particular sea snail fisheries, have constituted a frontier of sorts open to the poorer populations of Samsun during the last 20 years, and, thereby, constitute one of the major drivers for fishing pressure. We identify eight drivers of importance for the period 2000–2005. Although the authorities can impact all or most of those drivers, most of them are beyond the scope of conventional ‘fisheries management’. 相似文献