Climatic Variability and Agricultural Season: Analysis of the Evolution of Essential Agroclimatic Parameters in Central East Cote D’ivoire
Abstract
The relationships between rainfall indices and the increase in agricultural production in Côte d'Ivoire over the period 1980-2010 do not show significant results of the current climatic trends. The study of the beginnings of the agricultural season of the "old cocoa-loop" highlights the rainfall variations that have persisted since the 1970s, and exposes rainfed agriculture to climatic risks. In addition, both daily and seasonal rainfall data collected from 1961 to 2010 were analyzed to reveal the current rainfall trends. It is worth to note that the simple study of the chronological series of the effective installation of precipitations shows botha delay and sudden fluctuation of the agricultural seasons throughout the region under investigation, at the end of the 1960s and the beginning of the 1970s. Other variables such as "the duration and the end" of the season, allow a more "qualitative" characterization of the investigated phenomenon. They provide additional information regarding both the manifestations of the rainfall variability and the confirmation of the importance of the phenomenon. The risks to which rainfed agriculture is exposed in relation to the current rainfall conditions are: disruption of the agricultural cycle, loss of seeds, and reduction in yield.
Keywords
Download Options
Introduction
Agriculture is no longer the main source of money income in many rural areas of West Africa owing to the low agricultural productivity due to climatic hazards. Even with the gradual return of rainfall, it is probable that this trend will continue. Climatic hazards are areal concern for all West African countries owing to their adverse socio-economic and environmental effects. Interannual fluctuations in rainfall represent the main climatic hazard for West African countries such as Côte d'Ivoire, whose economy is principally based on agriculture [1]. This is of the pluvial type, i.e. dependent on rain, which is the most variable climatic element. The decline in rainfall that began in the Gulf of Guinea countries at the end of the 1970s, became more intense in Côte d'Ivoire during the 1980s and 1990s before experiencing a certain remission during the 2000s [2,10]. Thus, these rainfall recessions induce variability in agricultural calendars through the variation of start and end dates, as well as the duration of the seasons [3,9]. Therefore, the fundamental question that emanates from these observations is the following: what are the variations of the major agroclimatic parameters in the Center-East of Côte d'Ivoire? Thus, this study aims to show the modifications of the major agroclimatic parameters of the agricultural calendars in the Center-East of Côte d'Ivoire between 1971 and 2020. Once prosperous and a major center of rural immigration, the east-central part of Côte d'Ivoire has experienced an inversion of the situation in recent years, which has made it an important center of emigration. The decline in planting activity can be observed both in terms of areas and in terms of production [4,9]. In recent decades, the Center-East of Côte d'Ivoire has suffered a drop in rainfall marked by droughts [5,10]. The economic consequences of such climatic and ecological changes are dramatic in this region mainly oriented towards farming [6]. The irregularity of the temporal distributions of precipitations and the heterogeneity of their spatial distribution constitute today the essential characteristics of the pluviometry of this region. The analysis of rainfall over the three sub-periods 1971-2000, 1981-2010 and 1991-2020 shows that agriculture has been going through a rainfall crisis for five decades now. The typical aspects of rainfall variability are its persistence and amplitude [7]. The impact of this phenomenon has been observed through the drying up of the majority of water points, the rotting of seedlings, a reduction in arable land, lower yields and the resurgence of diseases (human, plant and animal). .Thus, entire regions have become more vulnerable than in the past, thus weakening their agricultural future and accentuating the process of deforestation [8]. In addition, this has imposed on them transformations in their lifestyles, regardless of the economic sector considered [9,7]. These characteristics give the climate a determining role in the development of the agricultural season and in agricultural production. Thus, given their immediate and lasting repercussions on agriculture and on humans. This variability leads to great uncertainty on the date of sowing which, on the same site, can occur over a period of nearly two months depending on the onset of the rains [10]. Our interest as a geographer aims to assess the extent of the evolution of rainfall in the Center-East in order to reveal its influence on the agricultural season. In agriculture, it has been shown that farmers who are convinced of the existence of climate variability have better capacities to manage risk and change. They are likely to anticipate it, learn and organize themselves and they are more willing to modify their systems [8,9]. Hence, an understanding of this climatic phenomenon could at least help to program interventions aimed at stabilizing and increasing yields [11].
Conclusion
The study of the evolution of the rainfall regime in the former Cacao loop in Côte d'Ivoire shows that seasonal variations are associated with a modification of agroclimatic parameters such as the beginning, the end and the duration of the agricultural season. There is a decrease in the length of the season, which has gone from 4 months to 3 months, a delay in the effective onset of the rains and a virtual disappearance of the short rainy season. End of season dates vary little in space and time. While it was believed for along time to be confined to the savannah region, this analysis showed that the rainfall deficit also affected the forest regions and, more generally, the so-called "wet" region. This fall in rainfall has, of course, consequences on the regimes of watercourses and therefore on the availability of water resources, key to the success of many development projects.