2013
DOI: 10.1016/s0187-6236(13)71090-7
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Modeling the potential impact of climate change in northern Mexico using two environmental indicators

Abstract: RESUMENLa modelación de impactos locales, caracterizados por deterioro de los recursos naturales -especialmente agua y suelo-ante los efectos globales del cambio climático, se ha convertido en una poderosa herramienta en la búsqueda de medidas de mitigación y adaptación. Los objetivos de la presente investigación fueron: 1) evaluar mediante procesos de modelación el impacto potencial del cambio climático para el periodo 2010-2039 y 2) advertir sobre riesgos futuros a partir de la identificación de forzantes ra… Show more

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Cited by 5 publications
(9 citation statements)
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“…The calculation and modeling of the LWER is based on the methodology proposed by SEDESOL-INE (1998) for studies of ecological land management (SELM) and has been used by López-Santos et al ( 2013 ) to model local impacts of climate change in northern Mexico according to four types of probable soil loss in ton per hectare per year: (1) light, <10; (2) moderate, 10–50; (3) high, 50–200; and (4) high, >200. This classification is set by the availability of environmental moisture following rainfall.…”
Section: Methodsmentioning
confidence: 99%
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“…The calculation and modeling of the LWER is based on the methodology proposed by SEDESOL-INE (1998) for studies of ecological land management (SELM) and has been used by López-Santos et al ( 2013 ) to model local impacts of climate change in northern Mexico according to four types of probable soil loss in ton per hectare per year: (1) light, <10; (2) moderate, 10–50; (3) high, 50–200; and (4) high, >200. This classification is set by the availability of environmental moisture following rainfall.…”
Section: Methodsmentioning
confidence: 99%
“…This classification is set by the availability of environmental moisture following rainfall. In addition, AI was calculated by De Martonne’s index, which has been used for the drylands of northern Mexico in several studies (Salinas-Zavala et al 1998 ; López-Santos et al 2013 ), to indicate drought (see “ Aridity index as an indicator of drought ” section).…”
Section: Methodsmentioning
confidence: 99%
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“…Además, se utilizó la Red Nacional de Estaciones Estatales Agroclimatológicas, Agroclima (10) del Instituto Nacional de Investigaciones, Forestales, Agrícolas y Pecuarias (INIFAP) para obtener datos de las temperaturas máxima, mínima y media, así como de humedad relativa (HR) para el municipio de Jesús María; con base en ello, se analizó la relación de las variables con el desarrollo poblacional de M. domestica y su posible infestación en el área de estudio. Los datos climáticos se interpolaron por el método basado en el inverso de la distancia ponderada (IDW, por sus siglas en inglés), el cual es descrito y aplicado en casos semejantes por diversos autores (11,12) .…”
Section: Materials Y Métodosunclassified