Volume 15, Issue 2, June 2015, Pages 287–295
Richard BIRINDWA CUBWE1, John KASHINZWE KIBEKENGE2, and Sylvain KULIMUSHI MATABARO3
1 Département de Géographie, Section des Sciences Exactes, Institut Supérieur Pédagogique de Walungu, RD Congo
2 Département de Géographie, Section des Sciences Exactes, Institut Supérieur Pédagogique de Walungu, RD Congo
3 Département de Géographie, Section des Sciences Exactes, Institut Supérieur Pédagogique de Walungu, RD Congo
Original language: French
Copyright © 2015 ISSR Journals. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
The present work proposes the determination of the rainy thermical rhythm in three parts in Luhwindja based on the North, Center and South which has not been known for a long time.
The south area of Luhwindja is better watered to some extent with 1753mm of water a year and the more less hot has got the everage yearly temperature of 17.4 degree centigrade. As the matter of fact three is not any month which is dry and scows can be transcorried the whole year; the monthly "ETP" being inferior to precipitations of all the twelve months of a year.
The North's area of Luhwindja with a yearly rainy thermical of 1553mm the everage temperature is 19.2 degree centigrade. It is the part less watered with three months which are affected by atmospherically drought during (June, July and August) are affected by pedological drougth; the "ETP" being superior to precipitations for the three dry months.
The Center receives on the one hand, precipitations coming from the North and on the other hand those of the South. It realizes 1611mmof water per a year and an everage temperature of 20.5 degree centigrade with three months affectedby atmospherically drought (June, July and August).
On average the whole Collectivity of Luhwindja receives 1639mm of water per year and a temperature of 19, 03 degree centigrade.
Author Keywords: Measure-Rainy thermical, LUHWINDJA.
Richard BIRINDWA CUBWE1, John KASHINZWE KIBEKENGE2, and Sylvain KULIMUSHI MATABARO3
1 Département de Géographie, Section des Sciences Exactes, Institut Supérieur Pédagogique de Walungu, RD Congo
2 Département de Géographie, Section des Sciences Exactes, Institut Supérieur Pédagogique de Walungu, RD Congo
3 Département de Géographie, Section des Sciences Exactes, Institut Supérieur Pédagogique de Walungu, RD Congo
Original language: French
Copyright © 2015 ISSR Journals. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Abstract
The present work proposes the determination of the rainy thermical rhythm in three parts in Luhwindja based on the North, Center and South which has not been known for a long time.
The south area of Luhwindja is better watered to some extent with 1753mm of water a year and the more less hot has got the everage yearly temperature of 17.4 degree centigrade. As the matter of fact three is not any month which is dry and scows can be transcorried the whole year; the monthly "ETP" being inferior to precipitations of all the twelve months of a year.
The North's area of Luhwindja with a yearly rainy thermical of 1553mm the everage temperature is 19.2 degree centigrade. It is the part less watered with three months which are affected by atmospherically drought during (June, July and August) are affected by pedological drougth; the "ETP" being superior to precipitations for the three dry months.
The Center receives on the one hand, precipitations coming from the North and on the other hand those of the South. It realizes 1611mmof water per a year and an everage temperature of 20.5 degree centigrade with three months affectedby atmospherically drought (June, July and August).
On average the whole Collectivity of Luhwindja receives 1639mm of water per year and a temperature of 19, 03 degree centigrade.
Author Keywords: Measure-Rainy thermical, LUHWINDJA.
Abstract: (french)
Le présent travail se propose de déterminer le rythme pluviothérmique dans trois parties de la Chefferie de Luhwindja (le Nord, le Centre et le Sud) longtemps inconnu pourtant important pour les activités agropastorales en milieu surtout rural.
Le Sud de la chefferie de Luhwindja est mieux arrosé avec 1753mm d'eau par an et le moins chaud avec une température moyenne annuelle de 17,4°C. Aucun mois n'est sec et les végétaux peuvent être verdoyants toute l'année, les ETP mensuelles étant inférieures aux précipitations tous les douze mois de l'année.
Le Nord de ladite Chefferie avec un total pluviométrique annuel de 1553mm d'eau et une température moyenne annuelle de 19,2°C est la partie la moins arrosée avec trois mois affectés de la sécheresse atmosphérique (Juin, Juillet et Aout) dont deux mois (Juillet et Aout) affectés de la sécheresse pédologique ; les ETP étant supérieures aux précipitations pour les trois mois secs.
Le Centre reçoit d'une part les précipitations venant du Nord et d'autre part celles du Sud. Il totalise 1611mm d'eau par an et une température de 20,5°C avec trois mois affectés de la sécheresse atmosphérique (Juin, Juillet et Aout).
En moyenne, toute la Chefferie de Luhwindja reçoit 1639mm d'eau par an et une température de 19,03°C.
Author Keywords: Mesure-pluviothérmique, LUHWINDJA.
How to Cite this Article
Richard BIRINDWA CUBWE, John KASHINZWE KIBEKENGE, and Sylvain KULIMUSHI MATABARO, “MESURES PLUVIOTHERMIQUES DE LA COLLECTIVITE-CHEFFERIE DE LUHWINDJA (2011),” International Journal of Innovation and Scientific Research, vol. 15, no. 2, pp. 287–295, June 2015.
