Application of a land surface model including fog deposition by a tree heath-laurel forest in the Garajonay National Park (La Gomera, Spain)

  1. Genki Katata 2
  2. Carlos M. Regalado 3
  3. Axel Ritter 1
  4. Haruyasu Nagai 2
  1. 1 Universidad de La Laguna
    info

    Universidad de La Laguna

    San Cristobal de La Laguna, España

    ROR https://ror.org/01r9z8p25

  2. 2 Japan Atomic Energy Agency
    info

    Japan Atomic Energy Agency

    Tōkai-mura, Japón

    ROR https://ror.org/05nf86y53

  3. 3 Instituto Canario de Investigaciones Agrarias
    info

    Instituto Canario de Investigaciones Agrarias

    San Cristóbal de La Laguna, España

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Actes de conférence:
Jornadas de Investigación de la Zona no Saturada del Suelo. ZNS'09: Estudios de la Zona No Saturada del Suelo, Vol. IX - ZNS’09 (9ª. 2009. Barcelona)
  1. Orlando Silva Rojas (ed. lit.)
  2. Jesús Carrera Ramírez (ed. lit.)

Éditorial: CIMNE

ISBN: 978-84-96736-83-2

Année de publication: 2009

Pages: 393-400

Type: Communication dans un congrès

GOOGLE SCHOLAR

Résumé

Se aplicó un modelo unidimensional multicapa atmósfera-suelo-vegetación (SOLVEG) que incluyedeposición de agua atmosférica (niebla). El modelo permitió cuantificar la distribución del contenido dehumedad en la zona no saturada y la cantidad de niebla interceptada que llega a la superficie del suelo de unacuenca de laurisilva en el Parque Nacional de Garajonay (La Gomera, España). El modelo permite dar cuentatanto de la deposición de agua atmosférica sobre hojas lanceoladas, como la captación de niebla por hojasaciculadas en un bosque mixto de fayal-brezal. El modelo se evaluó comparando medidas de contenido de aguaen el horizonte superficial del suelo y de transpiración con las predicciones del modelo SOLVEG obtenidas apartir de registros de variables micrometeorológicas y de captura artificial de niebla. El aporte anual de aguade niebla al suelo se estima en 110 mm, lo que equivale a un 18% de la precipitación. Es necesario, sinembargo, seguir investigando para reducir la incertidumbre de los parámetros del modelo y estimar así conmayor fiabilidad la contribución del agua de niebla al bosque de laurisilva

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