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Artykuły w czasopismach na temat "Multiannual dataset"
Rust, William, John P. Bloomfield, Mark Cuthbert, Ron Corstanje i Ian Holman. "The importance of non-stationary multiannual periodicities in the North Atlantic Oscillation index for forecasting water resource drought". Hydrology and Earth System Sciences 26, nr 9 (11.05.2022): 2449–67. http://dx.doi.org/10.5194/hess-26-2449-2022.
Pełny tekst źródłaGuðmundsson, Kristinn, Mike R. Heath i Elizabeth D. Clarke. "Average seasonal changes in chlorophyll a in Icelandic waters". ICES Journal of Marine Science 66, nr 10 (13.08.2009): 2133–40. http://dx.doi.org/10.1093/icesjms/fsp208.
Pełny tekst źródłaSaviano, Simona, Anastasia Angela Biancardi, Marco Uttieri, Enrico Zambianchi, Luis Alberto Cusati, Andrea Pedroncini, Giorgio Contento i Daniela Cianelli. "Sea Storm Analysis: Evaluation of Multiannual Wave Parameters Retrieved from HF Radar and Wave Model". Remote Sensing 14, nr 7 (31.03.2022): 1696. http://dx.doi.org/10.3390/rs14071696.
Pełny tekst źródłaSaviano, Simona, Anastasia Angela Biancardi, Florian Kokoszka, Marco Uttieri, Enrico Zambianchi, Luis Alberto Cusati, Andrea Pedroncini i Daniela Cianelli. "HF Radar Wind Direction: Multiannual Analysis Using Model and HF Network". Remote Sensing 15, nr 12 (8.06.2023): 2991. http://dx.doi.org/10.3390/rs15122991.
Pełny tekst źródłaPommier, C., C. Michotey, G. Cornut, P. Roumet, E. Duchêne, R. Flores, A. Lebreton i in. "Applying FAIR Principles to Plant Phenotypic Data Management in GnpIS". Plant Phenomics 2019 (30.04.2019): 1–15. http://dx.doi.org/10.34133/2019/1671403.
Pełny tekst źródłaWu, Tonghua, Changwei Xie, Xiaofan Zhu, Jie Chen, Wu Wang, Ren Li, Amin Wen i in. "Permafrost, active layer, and meteorological data (2010–2020) at the Mahan Mountain relict permafrost site of northeastern Qinghai–Tibet Plateau". Earth System Science Data 14, nr 3 (21.03.2022): 1257–69. http://dx.doi.org/10.5194/essd-14-1257-2022.
Pełny tekst źródłaShahi, Sonika, Jakob Abermann, Georg Heinrich, Rainer Prinz i Wolfgang Schöner. "Regional Variability and Trends of Temperature Inversions in Greenland". Journal of Climate 33, nr 21 (1.11.2020): 9391–407. http://dx.doi.org/10.1175/jcli-d-19-0962.1.
Pełny tekst źródłaDIMITROV, B. D., i E. S. BABAYEV. "Cyclic variations in the dynamics of flu incidence in Azerbaijan, 1976–2000". Epidemiology and Infection 143, nr 1 (18.03.2014): 13–22. http://dx.doi.org/10.1017/s095026881400048x.
Pełny tekst źródłaChiriaco, Marjolaine, Jean-Charles Dupont, Sophie Bastin, Jordi Badosa, Julio Lopez, Martial Haeffelin, Helene Chepfer i Rodrigo Guzman. "ReOBS: a new approach to synthesize long-term multi-variable dataset and application to the SIRTA supersite". Earth System Science Data 10, nr 2 (23.05.2018): 919–40. http://dx.doi.org/10.5194/essd-10-919-2018.
Pełny tekst źródłaLatchmore, Tessa, Paul D. Hynds, R. Stephen Brown, Kevin McDermott i Anna Majury. "Estimating the duration and overlap of Escherichia coli contamination events in private groundwater supplies for quantitative risk assessment using a multiannual (2010–2017) provincial dataset". Environmental Pollution 309 (wrzesień 2022): 119784. http://dx.doi.org/10.1016/j.envpol.2022.119784.
Pełny tekst źródłaRozprawy doktorskie na temat "Multiannual dataset"
Audoux, Thomas. "Approches expérimentales pour l’étude et la caractérisation des dépôts humides d’aérosols atmosphériques par les précipitations". Electronic Thesis or Diss., Université Paris Cité, 2022. http://www.theses.fr/2022UNIP7332.
Pełny tekst źródłaIn the work conducted for my thesis, I studied atmospheric aerosols and their transfer from the atmosphere to the surface by precipitation. The main strategy I followed is based on the observation of wet deposition on different time scales, interannual on one hand and intra-event on the other. It also relies on their observation in environments marked in terms of aerosol load and composition, but also in terms of atmospheric dynamics and precipitation. Combining measurements on both atmospheric and wet deposition compositions allows to identify the characteristics of the deposition (intensity, composition, source and origin) and to explain the phenomena involved in the deposition. This requires the complete documentation of different parameters (aerosols, dynamics, rainfall, deposition) over the same periods of time, which is nevertheless complex to implement. The two axes of my work deal with distinct and complementary issues in the study of wet deposition.The first focus has been on wet deposition in the Sahel, a semi-arid region where the scavenging of mineral dust from the atmosphere is a key process to constrain the atmospheric mass balance of these compounds. In this region marked by the presence of numerous convective systems controlling annual precipitation amounts, the question of the links between atmospheric dynamics and deposition was addressed. The long-term observation strategy implemented at stations in the Sahel as part of the INDAAF network, with a synergy of meteorological measurements, aerosol concentrations and deposition, has enabled the creation of a very complete database. From this multi-year dataset at Banizoumbou (Niger) and Cinzana (Mali) stations from 2007 and 2015, the identification of cold pools phenomena from surface meteorological data and their link with mineral dust deposition are discussed. Washout ratios have been calculated for cold pool events and vary over several orders of magnitude depending on the dilution effect which differs according to the levels of atmospheric aerosol concentrations. The most convective events associated with high concentrations have a less scattered range of values (319 – 766) that does not depend on the amount of precipitation.The second axis focused on the intra-event study of wet deposition in urban areas for various rainfall situations, aerosol concentration and composition. The question is: what can we learn from the monitoring of deposition during a rain event? To answer this, I first participated in the development of a collector allowing me to collect wet deposition in successive fractions during the rain event. Complemented by a set of co-located measurements on aerosols and atmospheric dynamics acquired in the field for 8 study cases, the chemical analyses of dissolved and particulate deposition allowed me to discuss both the origin of the aerosols and processes involved. I was able to quantify the decay of concentrations, even of trace compounds, in the deposits during rainfall. I was also able to document the evolution of solubility for chemical species in the deposition and discuss the relative contribution of the rainout and washout mechanisms. The variability of deposition observed during an event is actually as significant as that observed between rain events