Chad: Climate

Temperature

Figure 2: Air temperature projections for Chad for different GHG emissions scenarios.4

In response to increasing greenhouse gas (GHG) concentrations, air temperature over Chad is projected to rise by 2.1 to 4.3 °C (very likely range) by 2080 relative to the year 1876, depending on the future GHG emissions scenario (Figure 2). Compared to pre-industrial levels, median climate model temperature increases over Chad amount to approximately 2.1 °C in 2030 and 2.5 °C in both 2050 and 2080 under the low emissions scenario RCP2.6. Under the medium / high emissions scenario RCP6.0, median climate model temperature increases amount to 2.1 °C in 2030, 2.6 °C in 2050 and 3.5 °C in 2080.

Very hot days

Figure 3: Projections of the annual number of very hot days (daily maximum temperature above 35 °C) for Chad for different GHG emissions scenarios.

In line with rising mean annual temperatures, the annual number of very hot days (days with daily maximum temperature above 35 °C) is projected to rise with high certainty all over Chad (Figure 3). Under the medium / high emissions scenario RCP6.0, the multi-model median, averaged over the whole country, projects 17 more very hot days per year in 2030 than in 2000, 31 more in 2050 and 49 more in 2080. In some parts, especially in central Chad, this amounts to more than 300 days per year by 2080.

Precipitation

Figure 4: Annual mean precipitation projections for Chad for different GHG emissions scenarios, relative to the year 2000.

Future projections of precipitation are less certain than projections of temperature change due to high natural year-to-year variability (Figure 4). Out of the four climate models underlying this analysis, one model projects a decreasing trend in mean annual precipitation over Chad, one projects no change and two models project strong increases under RCP6.0. Compared to year 2000, median model projections show an increase in mean annual precipitation by 32 mm under RCP2.6 and 50 mm under RCP6.0 until 2080.

Heavy precipitation events

Figure 5: Projections of the number of days with heavy precipitation over Chad for different GHG emissions scenarios, relative to the year 2000.

In response to global warming, heavy precipitation events are expected to become more intense in many parts of the world due to the increased water vapour holding capacity of a warmer atmosphere. At the same time, the number of days with heavy precipitation events is expected to increase. This tendency is also found in climate projections for Chad (Figure 5), with climate models projecting an increase in the number of days with heavy precipitation, from 7 days per year in 2000 to 9 and 10 days per year in 2080 under RCP2.6 and RCP6.0, respectively.

Soil moisture

Figure 6: Soil moisture projections for Chad for different GHG emissions scenarios, relative to the year 2000.

Soil moisture is an important indicator for drought conditions. In addition to soil parameters and management, it depends on both precipitation and evapotranspiration and therefore also on temperature, as higher temperatures translate to higher potential evapotranspiration. Annual mean top 1-m soil moisture projections for Chad show almost no change under either RCP by 2080 compared to the year 2000 (Figure 6). However, there is considerable modelling uncertainty, as different hydrological models project different directions of change, which makes it difficult to identify a clear trend.

Potential evapotranspiration

Figure 7: Potential evapotranspiration projections for Chad for different GHG emissions scenarios, relative to the year 2000.

Potential evapotranspiration is the amount of water that would be evaporated and transpired if sufficient water was available at and below the land surface. Since warmer air can hold more water vapour, it is expected that global warming will increase potential evapotranspiration in most regions of the world. In line with this expectation, hydrological projections for Chad indicate a stronger rise of potential evapotranspiration under RCP6.0 than under RCP2.6 (Figure 7). Under RCP6.0, potential evapotranspiration is projected to increase by 2.1 % in 2030, 3.3 % in 2050 and 5.7 % in 2080 compared to year 2000 levels.

4 Changes are expressed relative to year 1876 temperature levels using the multi-model median temperature change from 1876 to 2000 as a proxy for the observed historical warming over that time period.