Abstract

In most (sub)-tropical African cultivated regions, more than one cropping cycle exists following the (one or two) rainy seasons. During the dry season, an additional cropping cycle is possible when irrigation is applied, which could result in 3 cropping seasons. In most agro-hydrological model applications such as SWAT+ in Africa, only one cropping season per year is represented. In this paper, we derived dynamic and static trajectories from seasonal land-use maps to represent the land- use dynamics following the major growing seasons, for the purpose of improving simulated blue and green water consumption from simulated evapotranspiration (ET) in SWAT+. This study builds upon earlier research that proposed an approach on how to incorporate seasonal land use dynamics in the SWAT+ model but mainly focused on the temporal pattern of LAI and tested the approach in a small catchment (240 km2). Together with information obtained from the cropping calendar, we implemented agricultural management operations for the dominant trajectory of each agricultural land-use class for the Kikuletwa basin (6650 km2 area coverage) in Tanzania. A comparison between the default SWAT+ (with static land use representation) set up, and a dynamic SWAT+ model (with seasonal land use representation) is done by spatial mapping of the evapotranspiration (ET) results. The results show that ET with seasonal representation is closer to remote sensing estimations, giving higher performance than default: the Root Mean Squared Error decreased from 181 to 69 mm/year; the percent bias decreased from 20 % to 13 % and Nash Sutcliffe Efficiency increased from −0.46 to 0.4. It is concluded that representation of seasonal land-use dynamics produces better ET results which provide better estimations of blue and green agricultural water consumption.

Highlights

  • 25 Representation of land-use dynamics in agro-hydrological models is important due to the numerous impacts of land-use changes on water resources (Wagner et al, 2019; Woldesenbet et al, 2017)

  • 80 This paper builds from previous work that proposed an approach on how to incorporate seasonal land use dynamics in Soil and Water Assessment Tool (SWAT) and SWAT+ models but was only evaluated for the temporal pattern of LAI simulations at a small catchment of 240 km2 (Nkwasa et al, 2020)

  • The monthly average ET value for the dynamic land-use scenario is closer to the remote sensing ET, especially during the dry months from July to November where we implement more than one cropping season

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Summary

Introduction

25 Representation of land-use dynamics in agro-hydrological models is important due to the numerous impacts of land-use changes on water resources (Wagner et al, 2019; Woldesenbet et al, 2017). Wagner et al, (2016) found a continuous decrease of annual evapotranspiration of up to -53mm (-7%) when dynamic land-use change is implemented per sub-basin scale. Most of these studies have implemented annual land-use dynamic. Since land-use refers to manmade socio-economic activities and management practices on the land, these anthropogenic activities 35 may change depending on a season, on cultivated land (Anderson et al, 1976). These changes per season are called seasonal land-use dynamics (Msigwa et al, 2019). The LAI dynamics of the seasonal landuse dynamic implementation showed more realistic temporal advancement patterns that corresponded to the seasonal rainfall within the basin

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