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Incorporation of prior information on parameters into nonlinear regression groundwater flow models. 1. Theory
  • Incorporation of prior information on parameters into nonlinear regression groundwater flow models. 1. Theory
American crop plants in Asia prior to European contact
  • American crop plants in Asia prior to European contact
Daily rainfall probabilities: conditional upon prior occurrence and amount of rain
  • Daily rainfall probabilities: conditional upon prior occurrence and amount of rain
The general linear model with prior information
  • The general linear model with prior information
EFFETS DES GRAVIERES SUR LE COMPORTEMENT HYDRODYNAMIQUE DES NAPPES D'EAU SOUTERRAINES
  • 1) BENEFICIAL AND ADVERSE EFFECTS OF EXCAVATION OF AN INCREASING NUMBER OF GRAVEL PITS IN ALLUVIAL FORMATION TO SUPPLY BUILDING MATERIAL AND BACKFILL. 2) HYDRODYNAMIC EFFECT OF THE FREE WATER IN THE PITS. INVESTIGATIONS REQUIRED PRIOR TO PROJECT
The interconnection of wetting and drying with freeze-thaw : some new data in Periglacial processes and landforms.
  • there was a velocity decrease. This velocity decrease is interpreted as being a consequence of changes in rock elasticity brought about by a diminution in the bonding strength of the rock. This means that wetting, prior to freezing, may weaken a rock.
Comparison of soils in midwestern United States and western Europe with the interglacial record
  • : widespread assumptions regarding greater warmth in interglaciations prior to the present one are generally unproven.
Recent seasonal rainfall and temperature relationships in peninsular Florida
  • . Autumn decrease in precipitation in the last two decades is apparently due to suppression of tropical cyclonic activity. The reverse of both of these trends was evident prior to the 1940s. These climatic patterns have resulted in seasonal redistribution
Stagnation or activity in the last ice remnants?
  • area must have decreased or partly ceased already when the eskers were formed on the hillsides. The drumlinization of the Rogen type ridges thus occurred at a stage prior to the disappearance of the ice bodies between the valley sides.
Geoarchaeological evidence for prairie-mound formation in the Mississippi alluvial valley, southeastern Missouri
  • Archaeological materials in several prairie mounds in the south-eastern Missouri indicate that mounds began forming prior to 5 000-3 000 yr B. P. The mounds subsequently were inundated and built up to their modern configuration by aggradational
The significance of stratified slope-waste deposits in the Quaternary of Umbria - Marche Apennines, Central Italy in Periglacial processes and landforms.
  • and eroded materials deposited prior to 0.25-0.29 MY. The second generation is related to terraced alluvial sediments| both deposits are strongly weathered to form a fersiallitic soil of Eemian age. This soil contains artifacts of the final Acheulean
Late Pleistocene climate and water budget of the South American Altiplano
  • Geomorphic evidence from the Peruvian-Bolivian Altiplano indicates that during episodes prior to 28,000 and around 12,500-11,000 yr BP lakes covered an area about six and four times as large as present, respectively. Within the constraints
Submarine landslides-geometry and nomenclature
  • PRIOR, D. B.
Landslide morphology and processes on some coastal slopes in Denmark and France in Coasts under stress.
  • PRIOR, D. B.
New faunal and isotopic evidence on the late Weichselian-Holocene oceanographic changes in the Norvegian Sea
  • Prior to oxygen-isotope termination IA (16,000-13,000 yr B.P.), an isolated watermass, with lower oxygen content and temperature warmer than today existed below a low salinity ice-covered surface layer in the Norwegian Sea. Close to termination IA
Major change in Atlantic deep and bottom waters 700,000 yr ago: benthonic foraminiferal evidence from the South Atlantic
  • ago. This rise indicates a sharp, sustained increase in the volume of bottom water flowing through the South Atlantic after this time. Prior to about 700,000 yr ago, the amount of Antarctic Bottom Water entering the western South Atlantic was greatly
Lateglacial environmental changes interpreted from fossil coleoptera from St. Bees, Cumbria, NW England in Studies in the Lateglacial of North-West Europe.
  • ... The Windermere (Lateglacial) Interstadial was at its warmest prior to 12,200 BP, and the climate was then somewhat warmer, at least during the summer, than at the present time... Deposits laid down during the Allerod period contain fossil
Observing long-period fluctuations of surface winds in the tropical Pacific: initial results from island data
  • A strengthening and subsequent weakening of the equatorial trades occurs prior to the first sea surface temperature anomaly at the coast of Peru, espacially in the Gilbert and Phoenix Island groups, for most of the El Nino events in 1950-1978
Patterns of carbon supply and distribution and oxygen renewal in two alaskan fjords in Sedimentology of fjords.
  • The deep basin water of Resurrection Bay (a simple-silled fjord at 60 N on the South central Alaskan coast) is renewed each summer with water having a dissolved oxygen concentration > 4 ml/l. Prior to 1976 more than 90 % of the allochtonous organic
Tropical stone lines and podzolized sand plains as paleoclimatic indicators for weathered cratons
  • Consideration of contemporary environments where the genetic processes related to these features can be observed, implies several conditions for prior events in landscape evolution: (1) tropical stone lines may be interpreted as winnowed mudflows