Cali - Analyseer mijn risico in 2 stappen

Selecteer focusgebied in Cali

The Cauca catchment is located in the mid-east part of Colombia and has Cali as its main urban area. The Cauca river flowing in a northern direction and is lying central in the catchment. The main type of land use and economic activity is agriculture (54%), but also the areas with nature are significant (33%). Population density is 567 persons/km2 and a large part of the population is rural. GDP is 7.285 (intermediate), but there is a significant level of poverty in the area. The Cali basin can be devided in six sub-basins: Rio Palo, Rio Guachal, Rio Claro, Rio Desbaratado, Rio Cali, and Rio Lili.

A sub-basin can be selected by clicking at the basin in the drop-down menu below. Once a sub-basin is selected it will appear in blue on the map.

Meer informatie over het Cali stromingsgebied

Rio Palo is the largest sub-basin, located in the upstream southern part of the Cauca basin. Its’ main type of land use and economic activity is agriculture (75%). Nature areas are also significant (23%), whereas no cities occur in the basin. Population density is low and a large part of the population is rural. GDP is relatively low and there is a significant level of (extreme) poverty in the area.

Rio Guachal is located the in the northeast of the Cauca basin and borders the Cauca river in the west. Its’ main type of land use and economic activity is agriculture (70%). Nature areas are also significant (27%), whereas urban area is small. Population density is low and a large part of the population is rural. GDP is intermediate, but there is a significant level of poverty in the area.

Rio Claro is located in the mid-west of the Cauca basin and borders the Cauca river in the east. Its’ main type of land use and economic activity is agriculture (58%). Nature areas are also significant (36%), whereas urban area is small. Population density is low and a large part of the population is rural. GDP is intermediate, but there is a significant level of poverty in the area.

Rio Desbaratado is a small sub-basin located in the mid-east of the Cauca basin and borders the Cauca river in the west. Its’ main type of land use and economic activity is agriculture (66%). Nature areas are also significant (33%), whereas urban area is very small. Population density is low and a large part of the population is rural. GDP is intermediate, but there is a significant level of poverty in the area.

Rio Cali is located in the northwest of the Cauca basin. The largest part of the sub-basin is covered with nature areas (55%), while agriculture land covers 28% of the area. The urban area is significant (almost 17%) with part of the city of Cali positioned in the sub-basin. Population density is high and a large part of the population is urban. GDP is relatively high, but there is also a significant level of poverty in the area.

Rio Lili is located in the northwest of the Cauca basin and borders the Cauca river in the east. The largest part of the sub-basin is covered with urban area (almost 55%) with a large part of the city of Cali positioned in the sub-basin. Agriculture land covers 24% of the area, while nature areas cover 21% of the area. Population density is high and a large part of the population is urban. GDP is relatively high, but there is also a significant level of poverty in the area.

 

Kies het toekomst scenario

Two future scenarios with changing climatic and socio-economic conditions were analysed for the São Paulo Basin: the rocky road scenario and the scenario of conventional development.

The rocky road scenario is based on SSP3, which is the sustainable shared socioeconomic pathway that represents a future with slow growth and fragmentation. The scenario of conventional development is based on SSP5. This is the socioeconomic pathway of conventional development that shows robust economic growth, but hampers sustainability and climate change mitigation.

For both scenarios the RCP8.5 climate scenario is used, which represents a worst case scenario: temperature rises, and precipitation increases during the wet seasons and decreases during the dry ones.

Meer info over scenariotypes

Climate scenario

For the purpose of WaterLOUPE future water shortage risk calculations, one RCP climate scenario was selected during the workshops: the RCP8.5 scenario. This climate scenario represents a worst-case scenario in which temperature increases, and precipitation increases during the wet seasons and decreases during the dry ones. This scenario was downscaled according to the approach that was followed for the Magdalena Basin (Colombia). Based on this approach, we translated this RCP into local water availability of the sub-basins.

In the last Assessment Report of IPCC (AR5), the approach to define the scenarios has focused on a parallel development of emissions and socioeconomic scenarios. The starting points of these scenarios are radiative forcing pathways that describe an emission trajectory and concentration by the year 2100. These radiative forcing trajectories are termed “Representative Concentration Pathways” (RCPs) and are broadly described as “climate scenarios”. The RCPs can either be or not be associated with unique socioeconomic and policy assumptions. They can also result from different combinations of economic, technological, demographic, policy, and institutional futures. There are four radiative forcing scenarios which are defined depending on the total radiative forcing in year 2100 relative to 1750. Scenario 2.6 is a mitigation scenario in which the emissions peak and decline before 2100. Scenarios 4.5 and 6.0 are stabilization scenarios and scenario 8.5 is a rising scenario with very high greenhouse gas emissions. The IPCC generated a set of data based on the new climate simulations carried out with the climate model ensemble under the framework of the Coupled Model Intercomparison Project Phase 5 (CMIP5) and using the RCPs as basis.

Socio-economic scenarios

The aim of the socio-economic scenarios is to understand how both exposure and vulnerability will develop in the future. Especially for the long-term horizon, it is impossible to predict socio-economic change; therefore, instead of using a single projection, we identify multiple scenarios that enable us to deal with different ‘what-if’ outcomes. As such, it is possible to design policy that is effective in different future outcomes.

In order to derive plausible socio-economic scenarios, the narratives and quantification of key drivers is derived from different global sources. Future population projections are derived from the United Nations and the IPCC (the ‘Shared-Socioeconomic Pathways’ – SSPs). The SSPs are also used for economic growth, sub-sectoral distribution and urbanization developments and directions of key vulnerability indicators. This is combined with local information on current abstractions of irrigation, households and industries in the relevant (sub-) catchments. Based on the different narratives, the future water demand distribution over different sectors and users is identified, as well as the vulnerability per user group. The narratives also include developments of legislation and regulation that influence water management. This is combined with different climate change scenarios to understand future risk under different scenarios for the different stakeholders in the catchment area. The following paragraph describes a short storyline per SSP.

SSP1 (Sustainability) represents a sustainable world where it is easy to mitigate and adapt to climate change because of the rapid development of low-income countries, reduced inequality, rapid technology development, and a high level of awareness regarding environmental degradation. Good yield enhancing technologies for agricultural land are also incorporated.

SSP2 (Middle of the Road) represents conditions where the socio-economic trends of recent decades continue. Reductions in resource use and energy intensity are achieved at historic rates.

SSP3 (Fragmentation or Rocky road) represents conditions where it is difficult to mitigate and adapt to climate change because of extreme poverty and a rapidly growing population. There is serious degradation of the environment, and technological change in the energy sector is slow. Because of the limited coordination between regions, use of local energy resources is enhanced.

SSP4 (Inequality) represents a highly unequal world both within and across countries. Crop yields would be high in industrial farming, but low for small scale farming.

SSP5 (Conventional Development) represents a situation where it is easy to adapt owing to robust economic growth, but difficult to mitigate the effects of climate change because the energy system is dominated by fossil fuels. Agro-ecosystems are highly managed, building on strong technological progress in the agricultural sector. Land use management is generally very resource intensive including the management of water systems.

References

A new scenario framework for Climate Change Research: scenario matrix architecture (2013)

Climate adaptation Colombia. Climate data scaling and analysis of the Magdalena basin (2014)

A new scenario framework for climate change research: the concept of shared socioeconomic pathways (2013)

Building global water use scenarios (2016)