{"query_echo":{"q":"","filters":{"analysis_type":["monitoring network design"]},"warnings":[{"code":"facet_value_not_in_vocabulary","message":"Value 'monitoring network design' for facet 'analysis_type' is not in the controlled vocabulary."}]},"total":{"value":2,"relation":"eq"},"page":1,"page_size":20,"self":"https://climateinsightsdirectory.org/api/v1/search?analysis_type=monitoring+network+design","stability":"beta","ai_marking":{"digital_source_type":{"uri":"http://cv.iptc.org/newscodes/digitalsourcetype/trainedAlgorithmicMedia","name":"Created using Generative AI"},"notice":"Summary and key insights are generated using artificial intelligence."},"results":[{"id":"wwfza-000020","url":"https://climateinsightsdirectory.org/document/wwfza-000020","title":"Establishing a citizen-science groundwater monitoring network for Constantia & Bergvliet, Western Cape","publisher":{"name":"WWF South Africa","organization":"wwf-south-africa"},"document_type":"report","language":"en","date_published":"2022-04-14","source_url":"https://wwfafrica.awsassets.panda.org/downloads/3_annexure_3_appendix_b_constantia_bergvliet.pdf","generator":"Climate Insights Directory","generated_fields":["summary","key_insights","climate_tags","geography_discussed","analysis_type"],"summary":{"text":"The report describes the creation of a groundwater monitoring network in Constantia and Bergvliet, Western Cape, commissioned by WWF South Africa. Following a significant increase in borehole drilling during the 2015-2019 drought, GEOSS South Africa conducted a desktop study and hydrocensus of 309 properties. The project resulted in the installation of five Solinst Leveloggers in private boreholes, with data fed into a public Groundwater Dashboard for the Table Mountain Water Source Area. Findings indicate that most boreholes target the Springfontyn and Peninsula Formations, with water levels ranging from 7 to 16 mbgl and quality classified as \"good\" to \"marginal\".","ai_generated":true,"unit":"wwfza-000020#summary","date_modified":"2026-10-23"},"key_insights":[{"text":"The 2015 to 2019 drought in the Western Cape and City of Cape Town led to a significant increase in the number of boreholes and wellpoints, as well as the volume of groundwater abstracted.","ai_generated":true,"unit":"wwfza-000020#insight-1","date_modified":"2026-10-23"},{"text":"A hydrocensus of 309 properties in Constantia and Bergvliet identified 41 boreholes and 11 wellpoints, with the majority drilled between 2016 and 2020 as a response to the drought.","ai_generated":true,"unit":"wwfza-000020#insight-2","date_modified":"2026-10-23"},{"text":"Boreholes in the study area typically range from 15 to 70 metres in depth, primarily targeting the fractured Peninsula Formation and the sandy soil of the Springfontyn Formation.","ai_generated":true,"unit":"wwfza-000020#insight-3","date_modified":"2026-10-23"},{"text":"Stakeholders expressed various concerns regarding groundwater, including the depletion of resources due to over-abstraction, high iron content in the water, and the potential for groundwater use to be taxed.","ai_generated":true,"unit":"wwfza-000020#insight-4","date_modified":"2026-10-23"},{"text":"A monitoring network consisting of five Solinst Leveloggers was deployed in private boreholes between February and March 2022, recording water levels between 7 and 16 mbgl.","ai_generated":true,"unit":"wwfza-000020#insight-5","date_modified":"2026-10-23"},{"text":"Groundwater quality in the study area, measured by electrical conductivity (EC), ranges from 40.8 to 82.5 mS/m, which is categorized as \"good\" to \"marginal\" according to DWAF (1998) guidelines.","ai_generated":true,"unit":"wwfza-000020#insight-6","date_modified":"2026-10-23"},{"text":"Monitoring data is manually downloaded and integrated into the Table Mountain Water Source Area Groundwater Dashboard to provide visibility of seasonal fluctuations and regional abstraction to stakeholders.","ai_generated":true,"unit":"wwfza-000020#insight-7","date_modified":"2026-10-23"}],"climate_tags":["drought","water security"],"geography_discussed":["Western Cape","City of Cape Town"],"frame_perspective":[],"analysis_type":["hydrogeological assessment","stakeholder engagement","monitoring network design"]},{"id":"wwfza-000185","url":"https://climateinsightsdirectory.org/document/wwfza-000185","title":"Establishing a citizen-science groundwater monitoring network for Scarborough & Kommetjie, Western Cape","publisher":{"name":"WWF South Africa","organization":"wwf-south-africa"},"document_type":"report","language":"en","date_published":"2022-04-14","source_url":"https://wwfafrica.awsassets.panda.org/downloads/3_annexure_3_appendix_d_scarborough_kommetjie.pdf","generator":"Climate Insights Directory","generated_fields":["summary","key_insights","climate_tags","geography_discussed","analysis_type"],"summary":{"text":"The report details the creation of a citizen-science groundwater monitoring network in Scarborough and Kommetjie, Western Cape, commissioned by WWF South Africa. Following a significant increase in borehole drilling during the 2015-2019 drought, the study employed desktop searches and a hydrocensus of 105 properties to identify groundwater users and monitoring sites. Four Solinst Leveloggers were deployed to track water levels and temperature, with data integrated into the Table Mountain Water Source Area Groundwater Dashboard. Findings indicate that borehole depths range from 1 to 60 metres, with water levels between 2.5 and 4 mbgl and electrical conductivity values between 54.8 and 150.7 mS/m. The report recommends continued stakeholder engagement and quarterly data downloads to ensure sustainable groundwater management.","ai_generated":true,"unit":"wwfza-000185#summary","date_modified":"2026-10-23"},"key_insights":[{"text":"The 2015 to 2019 drought in the Western Cape and City of Cape Town led to a significant increase in the number of boreholes and wellpoints, resulting in an unquantified rise in groundwater abstraction volumes.","ai_generated":true,"unit":"wwfza-000185#insight-1","date_modified":"2026-10-23"},{"text":"A hydrocensus of 105 properties in Scarborough and Kommetjie found that 27.6% of visited users completed surveys, identifying 12 boreholes and 17 wellpoints. Most of these were drilled between 2016 and 2020, suggesting they were a response to the drought.","ai_generated":true,"unit":"wwfza-000185#insight-2","date_modified":"2026-10-23"},{"text":"Borehole depths in the study area range from 1 to 60 metres. The targeted geological formations differ by location: quartzitic sandstones of the Peninsula Formation in Scarborough and sandy soils of the Springfontyn Formation in Kommetjie.","ai_generated":true,"unit":"wwfza-000185#insight-3","date_modified":"2026-10-23"},{"text":"Stakeholders expressed concerns regarding high iron content in the groundwater, as well as risks related to over-abstraction and the depletion of groundwater resources.","ai_generated":true,"unit":"wwfza-000185#insight-4","date_modified":"2026-10-23"},{"text":"A monitoring network consisting of four Solinst Leveloggers was deployed (three in boreholes and one in a well) between November 2021 and March 2022. Initial data shows rest water levels between 2.5 and 4 mbgl and electrical conductivity (EC) values between 54.8 and 150.7 mS/m.","ai_generated":true,"unit":"wwfza-000185#insight-5","date_modified":"2026-10-23"},{"text":"Monitoring data is manually downloaded and uploaded to the Table Mountain Water Source Area Groundwater Dashboard (groundwaterinfo.africa) to provide visibility of seasonal fluctuations and regional abstraction to stakeholders.","ai_generated":true,"unit":"wwfza-000185#insight-6","date_modified":"2026-10-23"}],"climate_tags":["drought","water security","water quality"],"geography_discussed":["Western Cape","City of Cape Town","South Africa"],"frame_perspective":[],"analysis_type":["hydrogeological assessment","stakeholder engagement","monitoring network design"]}]}