Climatic gradients along the windward slopes of Mount Kenya and their implication for crop risks. Part 1: Climate variability

Camberlin Pierre, Boyard-Micheau Joseph, Philippon Nathalie, Baron Christian, Leclerc Christian, Mwongera Caroline Njeri. 2014. Climatic gradients along the windward slopes of Mount Kenya and their implication for crop risks. Part 1: Climate variability. International Journal of Climatology, 34 (7) : pp. 2136-2152.

Journal article ; Article de revue à facteur d'impact
[img] Published version - Anglais
Access restricted to CIRAD agents
Use under authorization by the author or CIRAD.

Télécharger (1MB)


Liste HCERES des revues (en SHS) : oui

Thème(s) HCERES des revues (en SHS) : Géographie-Aménagement-Urbanisme-Architecture

Abstract : In tropical mountains, the way topographical gradients translate in terms of intra-seasonal and interannual climate variability (especially rainfall and evapotranspiration) is relatively unknown, yet it is an important issue for agriculture and food security. The eastern slopes of Mount Kenya, in East Africa, with their wide range of agro-ecological conditions, are appropriate for the study of these aspects. Daily (monthly) rainfall data from 11 (24) stations at different elevations and exposures are collected for the period 1961-2006. For the elevation belts suitable for farming and agro-pastoral activities, mostly below 2000 m, it is found that not all rainfall characteristics co-vary with altitude. Four distinct behaviours are revealed: (1) Parameters which show a relatively regular increase/decrease with elevation. This is the case for the duration of the two rainy seasons found across the region, and the mean onset and cessation dates, (2) Parameters which show a relatively uniform pattern throughout the region, with little differences both horizontally and vertically. This applies to the interannual variability of the October-December seasonal rains, which are quite homogeneously modulated by Indian Ocean sea-surface temperatures (SSTs), (3) Parameters markedly influenced by exposure. This applies to daily rainfall intensities, which peak along the southeast-facing slopes, whatever the altitude. The frequency of rainy days shows both a vertical gradient and some influence of exposure, (4) Parameters which show very weak spatial coherence, or pronounced vertical discontinuities. This is obvious for the cessation date of the March-May rains, whose poorly organized interannual variability contrasts with that of the onset. Variables involved in potential evapotranspiration (ET0) computation display either a strong (maximum temperature) or a weak (global radiation) vertical coherence, reflecting the existence/absence of an elevation control on the mean distribution of these variables. However, the interannual variations of global radiation have the strongest influence on those of ET0. (Résumé d'auteur)

Mots-clés Agrovoc : Terre en pente, Évapotranspiration, Climat de montagne, Saison humide, Variation saisonnière, Précipitation, Microclimat, Zone agroclimatique, Zone tropicale

Mots-clés géographiques Agrovoc : Kenya

Classification Agris : P40 - Meteorology and climatology

Champ stratégique Cirad : Axe 1 (2014-2018) - Agriculture écologiquement intensive

Auteurs et affiliations

  • Camberlin Pierre, CRC (FRA)
  • Boyard-Micheau Joseph, CRC (FRA)
  • Philippon Nathalie, Université de Bourgogne (FRA)
  • Baron Christian, CIRAD-ES-UMR TETIS (FRA)
  • Leclerc Christian, CIRAD-BIOS-UMR AGAP (FRA)
  • Mwongera Caroline Njeri, Montpellier SupAgro (FRA)

Source : Cirad - Agritrop (

View Item (staff only) View Item (staff only)

[ Page générée et mise en cache le 2021-03-08 ]