Hyllie Terrass · Transition modelFACILITY
MEASURED · confidence: 0.65 · status: activeClimate & nature exec summaryMalmö, SE · claude-sonnet-5 · 2026-07-07
Hyllie Terrass is a low-water-stress Malmö office asset riding Sweden's already near-decarbonised grid, with GHG and physical water risk both structurally low today.
Hyllie Terrass is a 14,000 sqm office asset in Malmö, Skåne, operating within the Baltic Sea watershed under a Low (<10%) baseline water stress label (BWS score 0.96) and a Low overall physical risk score of 0.44, with coastal and riverine flood scores both modest (1.13 and 1.32 respectively). Its dominant environmental dependency is grid electricity, and Sweden's 2025 observed grid intensity of 35.26 gCO2/kWh (Ember Yearly Electricity 2025) is already among the cleanest nationally, meaning Scope 2 emissions impact is comparatively low relative to peers on less-decarbonised grids. No flow-level consumption data (water, energy, waste) is recorded for the facility, limiting granular quantification of intensity today.
By 2030, Sweden's grid carbon intensity is projected to fall further to 25 gCO2/kWh (IEA WEO 2024 STEPS), continuing a decarbonisation path already well ahead of most European peers, meaning Scope 2 transition risk at this site remains negligible and improving. Water-related metrics show no populated 2030 horizon scores for water stress or depletion, so no forward shift in physical water risk can be evidenced from this dataset; the current Low overall risk score (0.44) and Low (<10%) baseline water stress label stand as the only reference points. The dominant shift through 2030 is therefore energy-side, not water-side.
By 2050, Sweden's grid is projected to fall to 15 gCO2/kWh under IEA WEO 2024 STEPS, essentially eliminating residual Scope 2 emissions risk for this office asset and leaving Skanska's transition exposure at Hyllie Terrass negligible from an energy-carbon standpoint. Physical risk trajectory is less certain: no 2050 or 2080 water stress, depletion, or drought horizon scores are populated in this dataset, so the durability of the current Low water-risk profile in the Baltic Sea basin cannot be confirmed beyond today's baseline. Absent updated horizon data, the facility should be treated as low residual risk on both decarbonisation and water dimensions, pending confirmation of long-range physical projections.
Flows0 total · 0 in / 0 out · plus site context + supply/downstream
0.96 · Low (<10%) · Baltic Sea (ex 641, 654, 656, 672, 673)