Thanks — Temperature buffering subsurface and/or deep urination

The indicator is an estimate of potential cold extraction from urination deeper than 10 meters for cooling of residential and residential areas, hospitals, computer centers, etc. In Dutch urban areas, 20-40 meters deep wells were dug for sand extraction, which then remained as a recreational lake. in summer, in these lakes at 5-8 meters depth, a temperature jump layer (thermocline) under which 5-10 °C cold water is preserved from the previous winter period. This cold primer can be used or used for cooling. Currently only cold is extracted from the Nieuwe Meer and the Ouderkerkerplas in the southern urban area of Amsterdam. The water boards shall grant the permit for cold extraction, which shall be tested for water quality, fish growth and monitoring of harmful forms of algal bloom, with the participation of stakeholders in the recreational use or usefulness of the lake. This map gives an example for three puddles around Amsterdam and only shows the direct cold extraction from puddles.本指标用于估算10米以下水体的潜在冷提取潜力，可应用于住宅区域、医院、计算机中心等场所的制冷需求。 在荷兰城市区域，曾开挖20至40米深的采砂井，后续这些井坑形成了休闲湖泊。夏季，这类湖泊5至8米深度处会形成温度跃层（thermocline），跃层下方储存着源自前一冬季的5至10摄氏度冷水。此类冷源可用于制冷。目前，阿姆斯特丹南部城区仅从新湖（Nieuwe Meer）与奥德尔凯克尔湖（Ouderkerkerplas）提取冷水。 水务管理机构应核发冷水提取许可，许可审批需开展水质、鱼类生长状况及有害藻华监测等相关评估，并需吸纳参与湖泊休闲利用的利益相关方参与决策。 本地图以阿姆斯特丹周边的三处水坑为例，仅展示了从水坑直接提取冷水的应用场景。