Zobrazeno 1 - 10
of 150
pro vyhledávání: '"Peter A. Dowd"'
Publikováno v:
Resources, Vol 13, Iss 3, p 42 (2024)
This paper describes the use of a unique spatio-temporally resolved precipitation and temperature dataset to assess the spatio-temporal dynamics of water resources over a period of almost seven decades across the Sierra Nevada mountain range, which i
Externí odkaz:
https://doaj.org/article/299e43ddb9a747618c4a2759aa0ce0c0
Autor:
Eulogio Pardo-Igúzquiza, Juan J. Durán-Valsero, Peter A. Dowd, Juan A. Luque-Espinar, Javier Heredia, Pedro A. Robledo-Ardila
Publikováno v:
International Journal of Geoheritage and Parks, Vol 10, Iss 2, Pp 196-217 (2022)
Closed depressions are scale-invariant landforms that are the most distinctive and characteristic landform in karst terrains at the millimetre-to-kilometre scales. The purpose of this paper is twofold. The first is to raise awareness of the geoherita
Externí odkaz:
https://doaj.org/article/8c54b9617bef4ccc8bce0ca07a4bc92f
Autor:
Eulogio Pardo-Igúzquiza, Jean-Philippe Montillet, José Sánchez-Morales, Peter A. Dowd, Juan Antonio Luque-Espinar, Neda Darbeheshti, Francisco Javier Rodríguez-Tovar
Publikováno v:
Hydrology, Vol 10, Iss 9, p 187 (2023)
This paper investigates the relationship between rainfall, groundwater and Gravity Recovery and Climate Experiment (GRACE) data to generate regional-scale estimates of terrestrial water storage variations in the Andalucía region of southern Spain. T
Externí odkaz:
https://doaj.org/article/7b7da24cecd44fe2bf09cd939404502d
Publikováno v:
International Journal of Speleology, Vol 48, Iss 1, Pp 11-20 (2019)
Many features of a karst massif can either be modelled using fractal geometry or have a fractal distribution. For the exokarst, typical examples include the geometry of the landscape and the spatial location and size-distribution of karst depressions
Externí odkaz:
https://doaj.org/article/942014a59c1d482a9ca48b36f9b9d2e3
Publikováno v:
Acta Carsologica, Vol 42, Iss 1 (2013)
Digital elevation models (DEM) are digital representations of topography that are especially suitable for numerical terrain analysis in earth sciences and engineering. One of the main quantitative uses of DEM is the automatic delineation of flow netw
Externí odkaz:
https://doaj.org/article/5f5f5d2ed1b74cc09ac3100f30a045d0
Publikováno v:
Mathematical Geosciences. 54:243-282
The objective of the work presented in this paper is to provide a quantitative measure of grade heterogeneity at the selective mining unit scale within relatively large estimated resource blocks. The purpose of the work is to provide a means of evalu
Autor:
Exequiel Sepúlveda, Amir Adeli, Peter A. Dowd, Julian M. Ortiz, Sultan Abulkhair, Chaoshui Xu
Traditional geostatistical simulation techniques rely on the assumption of multi-Gaussianity. Although the normal score transform is widely used to convert data to a Gaussian distribution, it only guarantees that the normal scores will be univariate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b99128646628462a57fc7319559882a
https://doi.org/10.21203/rs.3.rs-2087808/v1
https://doi.org/10.21203/rs.3.rs-2087808/v1
Autor:
Peter A. Dowd, Eulogio Pardo-Igúzquiza
Publikováno v:
Mathematical Geosciences. 53:1027-1045
Closed terrain depressions are geomorphic features that show scale invariance over the wide range of scales on which they occur, from metres to thousands of kilometres. They are also global features that are present on all continents. Morphometric an
One of the most challenging aspects of multivariate geostatistics is dealing with complex relationships between variables. Geostatistical co-simulation and spatial decorrelation methods, commonly used for modelling multiple variables, are ineffective
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6d656922e04c21b1285573d1c0eca197
Publikováno v:
Computers & Geosciences. 130:69-83
In rock physics and petrological applications, pore identification from cast thin-section (CTS) images is a widely used means of estimating porosity and evaluating types of pores and pore structure parameters. Common problems encountered in current a