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Observation Network (observation + network)

Distribution by Scientific Domains

Earth and Environmental Science	50%

Selected Abstracts

Three-dimensional spatial interpolation of surface meteorological observations from high-resolution local networks

METEOROLOGICAL APPLICATIONS, Issue 3 2008
Francesco Uboldi
Abstract An objective analysis technique is applied to a local, high-resolution meteorological observation network in the presence of complex topography. The choice of optimal interpolation (OI) makes it possible to implement a standard spatial interpolation algorithm efficiently. At the same time OI constitutes a basis to develop, in perspective, a full multivariate data assimilation scheme. In the absence of a background model field, a simple and effective de-trending procedure is implemented. Three-dimensional correlation functions are used to account for the orographic distribution of observing stations. Minimum-scale correlation parameters are estimated by means of the integral data influence (IDI) field. Hourly analysis fields of temperature and relative humidity are routinely produced at the Regional Weather Service of Lombardia. The analysis maps show significant informational content even in the presence of strong gradients and infrequent meteorological situations. Quantitative evaluation of the analysis fields is performed by systematically computing their cross validation (CV) scores and by estimating the analysis bias. Further developments concern the implementation of an automatic quality control procedure and the improvement of error covariance estimation. Copyright © 2008 Royal Meteorological Society [source]

Jacobian mapping between vertical coordinate systems in data assimilation

THE QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, Issue 627 2007
Y. J. Rochon
Abstract Radiances measured by remote-sensing instruments are now the largest component of the atmospheric observation network. The assimilation of radiances from nadir sounders involves fast radiative transfer (RT) models which project profiles provided by forecast models onto the observation space for direct comparison with the measurements. One of the features typically characterizing fast RT models is the use of a fixed vertical coordinate. If the vertical coordinate of the RT model is not identical to that used by the forecast model, an interpolation of forecast profiles to the RT model coordinate is necessary. In variational data assimilation, the mapping of the Jacobians (derivatives of the RT model output with respect to its inputs) from the RT model coordinate to the forecast model coordinate is also required. This mapping of Jacobians is accomplished through the adjoint of the forecast profile interpolator. As shown, the nearest-neighbour log-linear interpolator commonly used operationally can lead to incorrect mapping of Jacobians and, consequently, to incorrect assimilation. This incorrect mapping occurs as a result of leaving out intermediate levels in the interpolation. This problem has been previously masked in part through the smoothing effect of forecast-error vertical correlations on the analysis increments. To solve this problem, two simple versions of an interpolator relying on piecewise log-linear weighted averaging over the layers are investigated. Both markedly improve Jacobian mappings in the assimilation of observations, with one being slightly favoured over the other. This interpolator is being incorporated into the RTTOV model used by several operational weather forecasting centres. Copyright © 2007 Crown in the right of Canada. Published by John Wiley & Sons, Ltd. [source]

Hosts and distribution of Collybia fusipes in France and factors related to the disease's severity

FOREST PATHOLOGY, Issue 1 2002
D. PIOU
Using data collected by two different observation networks, it was possible to clarify the distribution of Collybia fusipes in France. It is frequently found in the western and northern parts of France, mainly on Quercus rubra and Quercus robur, and to a somewhat lesser extent on Quercus petraea. When the relative areas covered by these species are compared, it is evident that Q. rubra is much the most susceptible of the three species. The fungus has been less frequently reported in the south-eastern quarter of France, where Quercus ilex and Quercus pubescens are the dominant species. Complementary observations carried out at the National Arboretum of Les Barres indicate that a large number of oak species are susceptible to infection by this fungus, particularly those in the subgenus Erythrobalanus. These observations are discussed with reference to reports of this fungus throughout Europe. In a Q. rubra stand, fruit-body clumps were monitored and root damage was assessed on 73 final-crop trees and 40 codominant trees. The results suggest that C. fusipes does not preferentially infect weakened trees. Both the severity of root damage and the number of fruit-body clumps increased with increasing depth to signs of waterlogging. Répartition et hôtes de Collybia fusipes en France et facteurs de gravité de la maladie D'après les données collectées par deux réseaux de surveillance distincts, la répartition de Collybia fusipes en France a été précisée. Le champignon est fréquent dans les moitiés ouest et nord du pays, principalement sur Quercus rubra et Q. robur, et dans une moindre mesure sur Q. petraea. Quand on considère la surface relative occupée par ces espèces, il apparaît évident que Q. rubra est le plus sensible. Il a été moins souvent signalé dans le quart sud-est oùQ. ilex et Q. pubescens sont dominants. Des observations complémentaires réalisées à l'Arboretum National des Barres indiquent qu'un grand nombre d'espèces de chênes sont susceptibles d'être attaquées par ce champignon, particulièrement celles du sous-genre Erythrobalanus. Ces observations sont discutées et comparées avec les données disponibles en Europe. L'apparition des carpophores a été suivie dans un peuplement de Q. rubra, et les dégâts aux racines ont étéévalués sur 73 arbres de place et 40 arbres codominants. Les résultats indiquent que C. fusipes n'infecte pas plus gravement les arbres affaiblis. Le degré d'hydromorphie influence significativement l'importance des dégâts racinaires ainsi que le nombre de carpophores produits. Cette étude confirme que C. fusipes se développe préférentiellement dans les sites où l'hydromorphie n'est pas trop sévère. Wirtspflanzen und Verbreitung von Collybia fusipes in Frankreich sowie mit der Krankheitsintensität assoziierte Umweltfaktoren Mit Hilfe der Daten von zwei unterschiedlichen Beobachtungsnetzwerken konnte die Verbreitung von Collybia fusipes in Frankreich präzisiert werden. Der Pilz ist im Westen und Norden des Landes häufig auf Quercus rubra und Quercus robur zu finden, etwas weniger häufig auf Quercus petraea. Beim Vergleich der von diesen Arten bestockten Flächen wird deutlich, dass Q. rubra die anfälligste der drei Eichenarten ist. Im südöstlichen Teil Frankreichs, wo Quercus ilex und Quercus pubescens dominieren, wurde der Pilz weniger häufig nachgewiesen. Ergänzende Beobachtungen im Arboretum National des Barres ergaben, dass zahlreiche Eichenarten gegen C. fusipes anfällig sind, insbesondere die des Subgenus Erythrobalanus. Diese Ergebnisse werden im Vergleich mit der aus Europa über diesen Pilz verfügbaren Literatur diskutiert. In einem Q. rubra, Bestand wurde das Auftreten von Fruchtkörpern und von Wurzelschäden an 73 herrschenden und 40 mitherrschenden Bäumen registriert. Die Ergebnisse zeigen, dass C. fusipes geschwächte Bäume nicht bevorzugt befällt. Sowohl die Intensität der Wurzelschäden als auch die Anzahl der Fruchtkörper erhöhte sich mit zunehmender Tiefe der Anzeichen für Staunässe im Bodenprofil. [source]

Development of a historical ice database for the study of climate change in Canada

HYDROLOGICAL PROCESSES, Issue 18 2002
Frédéric Lenormand
Abstract The Canadian government has been compiling various observations on freshwater and coastal sea ice conditions for many years. However, the records are not easily accessible and are dispersed within different government departments. Given this, a major effort was undertaken in order to gather all available observations into a common database,the Canadian Ice Database (CID). This database will respond to the needs for climate monitoring in Canada, the validation and improvement of numerical ice models and the development of new remote-sensing methods. Indeed, several studies have shown that freshwater ice and sea ice are good proxy indicators of climate variability and change. The first version of CID contains in situ observations from 757 sites distributed across Canada, which were originally kept on digital or paper records at the Meteorological Service of Canada Headquarters and the Canadian Ice Service (CIS). The CID holds 63 546 records covering the period from ice season 1822,23 to 2000,01. An analysis of the database allows one to trace the temporal evolution of the ice networks. The freeze-up/break-up network of 2000,01 only represents 4% of what it was in 1985,86. A drastic decline of the ice thickness and the snow on ice network is also observable. In 1997,98, it represented only 10% of the network that existed in 1984,85. The major budget cuts in Canadian government agencies during the late 1980s and the 1990s offer the most plausible explanation for the drastic decline in the ice observation networks. Weekly ice coverage determination on large lakes from satellite imagery by the CIS and the national volunteer ice monitoring program, IceWatch, may provide a means of reviving, at least, the freeze-up/break-up network. Copyright © 2002 John Wiley & Sons, Ltd. [source]