0000000000043075

AUTHOR

Martin De Luis

0000-0002-7585-3636

showing 3 related works from this author

A global perspective on the climate‐driven growth synchrony of neighbouring trees

2020

2 .pdf files: File 1. Author's article final version, Post-Print (19 Pags.- 4 Figs.- 2 Tabls.). File 2. Supplementary Materials (3 Figs.- 2 Tabls.- 1 Model Equation).

0106 biological sciencesGlobal and Planetary ChangeEcologyForest dynamicsEcologytree stress indicator010604 marine biology & hydrobiologyGlobal warmingCovarianceCarbon sequestrationtree-ringglobal010603 evolutionary biology01 natural sciencesSynchronyProductivity (ecology)DendrochronologyEnvironmental sciencePhysical geographyPrecipitationTemperate rainforestEcology Evolution Behavior and Systematics
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Temperature variability in the Iberian Range since 1602 inferred from tree-ring records

2017

Abstract. Tree rings are an important proxy to understand the natural drivers of climate variability in the Mediterranean Basin and hence to improve future climate scenarios in a vulnerable region. Here, we compile 316 tree-ring width series from 11 conifer sites in the western Iberian Range. We apply a new standardization method based on the trunk basal area instead of the tree cambial age to develop a regional chronology which preserves high- to low-frequency variability. A new reconstruction for the 1602–2012 period correlates at −0.78 with observational September temperatures with a cumulative mean of the 21 previous months over the 1945–2012 calibration period. The new IR2Tmax reconstr…

lcsh:GE1-350Global and Planetary Changegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesStratigraphyLaglcsh:Environmental protectionPaleontology010502 geochemistry & geophysicsSolar irradiance01 natural sciencesMediterranean BasinBasal areaVolcanolcsh:Environmental pollutionPeninsulaClimatologylcsh:TD172-193.5Dendrochronologylcsh:TD169-171.8Geologylcsh:Environmental sciences0105 earth and related environmental sciencesChronology
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A regional analysis of the effects of largest events on soil erosion

2012

A large amount of geomorphic work is caused by a small number of extreme events that are mainly responsible for the time compression of geomorphic processes. The classic approach defines extreme events by their magnitude and they are quantified by certain deviation from a central value. Alternatively, we define extreme events as the largest events sorted by rank, whatever their absolute magnitude. In this case, events with equal rank from two different sites can be responsible for different magnitudes of geomorphic work, e.g., the amount of erosion. The new approach applied to soil erosion is that, whatever the magnitude of soil eroded, erosion is a time compressed process and the percentag…

Absolute magnitudeHydrologyUniversal Soil Loss EquationErosionTemperate climatePeriod (geology)Environmental scienceMagnitude (mathematics)Soil classificationScale (map)Earth-Surface ProcessesCATENA
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