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TROIB · Engineering Brief

Sea Water Air Conditioning for Coastal Data & Urban Loads

Florida OTEC plantships moored in the Gulf Stream export power to the grid and pipe post-turbine cold water ashore to a SWAC district loop — cooling downtown Miami carrier hotels, edge data centers, and high-rises at a fraction of mechanical-chiller energy.

Document No. TROIB-EB-03 Revision A Classification: Conceptual / Illustrative Date: 2026 DOI: pending · Zenodo

Abstract

Sea Water Air Conditioning (SWAC) uses naturally cold deep seawater as the chilled-water source for a district cooling network, displacing the electrically intensive vapour-compression chillers that dominate building energy in hot, humid coastal cities. In the TROIB Southeast Florida zone, utility OTEC plantships are moored 3–5 mi offshore in the Gulf Stream; they export firm power to the FPL grid through a high-voltage subsea cable, and their post-turbine cold water (already drawn from depth and warmed only to ≈7–10 °C) is piped to a mainland SWAC district loop serving downtown Miami carrier hotels, edge data centers, and high-rise HVAC. Because SWAC replaces compressor work with pumping work, cooling energy intensity falls from ≈0.6–0.9 kW/ton for conventional chillers to ≈0.1–0.2 kW/ton. This brief presents the loop heat-exchange basis, the tons-of-refrigeration accounting, and the district load-growth trajectory to a Year-10 offset of ≈250 MW of urban cooling alongside 600 MW of direct-to-grid power.

Plantship and Grid Architecture

The Florida zone uses purpose-moored OTEC plantships rather than re-used rigs. Stationed 3–5 mi offshore over the Florida Straits, each plantship sits in the Gulf Stream where warm surface water is reliably ≈25 °C and a cold-water pipe reaches ≈4 °C deep water. Two products leave the plantship: electricity, exported through a high-voltage subsea cable to a Florida Power & Light (FPL) shore station, and cold water, whose remaining thermal capacity is harvested ashore for district cooling rather than discharged.

This dual-use is the efficiency multiplier of the Florida zone. The cold seawater has already been pumped from depth — the dominant OTEC parasitic — so using its residual chill for air conditioning is nearly free incremental value. After passing the OTEC condenser the water has warmed only to roughly 7–10 °C, still far colder than any chilled-water loop a mechanical plant would produce.

The SWAC District Loop

Cold seawater is never circulated through customer buildings directly — corrosion and biofouling forbid it. Instead, a shoreside titanium plate heat exchanger transfers cold from the seawater stream to a closed freshwater district loop. That district loop distributes chilled water through insulated mains to building cooling stations, where a second heat exchanger serves the in-building HVAC. The seawater, now warmed, is returned to a benign mixing depth offshore.

Florida sea water air conditioning loop schematic showing an offshore OTEC plantship, a subsea cold-water and power route to shore, a shoreside heat exchanger, and a district chilled-water loop serving downtown Miami buildings.
Florida SWAC district-cooling loop. An offshore OTEC plantship exports power via HV subsea cable and sends post-turbine cold water (≈7–10 °C) ashore. A titanium plate heat exchanger couples the seawater to a closed freshwater district loop that cools downtown Miami carrier hotels, edge data centers, and high-rises, replacing mechanical chillers.

Energy: Compressors vs Pumps

A conventional building chiller runs a vapour-compression cycle: a compressor lifts heat from chilled water up to a hot outdoor condenser. That compressor is the energy cost, conventionally expressed in kilowatts of electricity per ton of refrigeration (1 ton = 3.517 kW of cooling). Efficient water-cooled chillers run ≈0.6 kW/ton; older or air-cooled units reach 0.9 kW/ton or worse.

SWAC has no compressor. The cold already exists in the deep sea; the only electrical cost is pumping seawater and circulating the district loop — on the order of 0.1–0.2 kW/ton. The energy reduction is therefore roughly 4–8×, as summarized in Table 1.

Illustrative cooling energy intensity: conventional chillers vs SWAC.
SystemMechanismEnergy intensityRelative
Air-cooled chillerVapour compression~0.9 kW/ton1.0×
Water-cooled chillerVapour compression~0.6 kW/ton0.67×
TROIB SWAC loopPumping only~0.1–0.2 kW/ton0.11–0.22×
3.517 kW
1 ton of refrigeration
~0.15 kW/ton
SWAC pumping intensity
250 MW
Urban cooling offset · Yr 10
600 MW
Direct-to-grid power · Yr 10

Loop Heat-Exchange Sizing

The cooling capacity a SWAC loop can deliver is fixed by the seawater flow it can move and the temperature rise allowed across the shoreside exchanger:

Q = ṁ · cp · ΔT

where Q is cooling power (kW), ṁ the seawater mass-flow rate (kg/s), cp ≈ 3.99 kJ/kg·K, and ΔT the seawater temperature rise across the heat exchanger. Converting the result to tons of refrigeration uses Q[tons] = Q[kW] / 3.517.

Worked example — district main

Suppose the shoreside exchanger draws seawater at ṁ = 3,000 kg/s and the seawater is allowed to warm by ΔT = 10 K (from ≈8 °C to 18 °C):

Q = 3,000 × 3.99 × 10 ≈ 119,700 kW ≈ 120 MWth
Q = 119,700 / 3.517 ≈ 34,000 tons of refrigeration

A single district main on the order of 3 m3/s of cold seawater therefore delivers roughly 120 MW of cooling — enough to serve a substantial cluster of downtown towers and data halls. The avoided compressor energy at ≈0.6 kW/ton would be near 20 MWe, which instead remains available as grid export.

District Load Growth

The Florida district cooling offset and direct-to-grid power scale together as plantship capacity and the shoreside distribution network expand. Table 2 gives the illustrative trajectory.

Illustrative Florida-zone load growth.
MilestoneUrban cooling offsetDirect-to-grid powerPrimary loads served
Year 3~40 MW~120 MWAnchor carrier hotels, pilot district
Year 6~130 MW~350 MWDowntown core, edge data centers
Year 10~250 MW~600 MWFull district + high-rise HVAC

By replacing roughly 250 MW of compressor-based cooling with pumping-only SWAC, the zone removes both the electrical demand and the urban waste-heat rejection of those chillers from a dense, heat-stressed coastal core — while the 600 MW of firm OTEC power feeds the FPL grid as zero-emission baseload.

Nomenclature

SWACSea Water Air Conditioning
QCooling (heat-exchange) power (kW)
Seawater mass-flow rate (kg/s)
cpSpecific heat of seawater (≈3.99 kJ/kg·K)
ΔTSeawater temperature rise across exchanger (K)
tonTon of refrigeration = 3.517 kW of cooling
kW/tonElectrical energy intensity of cooling
HVHigh-voltage (subsea export cable)
FPLFlorida Power & Light (grid offtaker)

Selected References (illustrative)

  1. International District Energy Association. District Cooling Best Practice Guide. Illustrative bibliographic entry.
  2. Makai Ocean Engineering. Sea Water Air Conditioning: System Design and Pipeline Engineering. Conceptual reference, illustrative.
  3. ASHRAE. Handbook — HVAC Systems and Equipment: District Cooling. Illustrative bibliographic entry.
  4. U.S. Department of Energy. Deep-Water Source Cooling for Coastal Urban Districts. Conceptual reference, illustrative.
  5. TROIB Project. Engineering Brief TROIB-EB-01: Closed-Cycle Ammonia OTEC. Companion document.