Global Ag-Climate Atlas
40 commercial greenhouse regions, ordered north to south. Each hub summarises latitude, Köppen climate class and seasonal natural Daily Light Integral (DLI, mol/m²/day) as a starting point for screen, lighting and heating design.
Bleiswijk, Netherlands
Maritime Temperate (Cfb)
- Summer DLI
- 34-40
- Winter DLI
- 6-9
Naaldwijk (Westland East), Netherlands
Maritime Temperate (Cfb)
- Summer DLI
- 35-41
- Winter DLI
- 6-10
Westland, Netherlands
Maritime Temperate (Cfb)
- Summer DLI
- 38-42
- Winter DLI
- 5.4-8.5
Straelen / Lower Rhine, Germany
Continental Transition (Cfb)
- Summer DLI
- 36-42
- Winter DLI
- 5-9
Nürnberg / Knoblauchsland, Bavaria
Warm-Summer Humid (Cfb)
- Summer DLI
- 38-45
- Winter DLI
- 7.2-10.5
Delta / Fraser Valley, BC, Canada
Pacific Maritime (Cfb)
- Summer DLI
- 36-44
- Winter DLI
- 6-11
Brittany (Finistère), France
Hyper-Maritime Cool Summer (Cfb)
- Summer DLI
- 32-38
- Winter DLI
- 7-11
Leamington / Kingsville, Ontario, Canada
Humid Continental (Dfa)
- Summer DLI
- 40-48
- Winter DLI
- 8-14
Morehead (Appalachian Basin), Kentucky, USA
Humid Subtropical (Cfa)
- Summer DLI
- 38-46
- Winter DLI
- 10-16
Murcia (Campo de Cartagena), Spain
Semi-Arid Mediterranean (BSk)
- Summer DLI
- 48-56
- Winter DLI
- 15-20
Antalya (Aksu & Kumluca), Turkey
Mediterranean Hot Summer (Csa)
- Summer DLI
- 50-58
- Winter DLI
- 16-22
Ragusa / Vittoria, Sicily, Italy
Hot Mediterranean (Csa)
- Summer DLI
- 52-60
- Winter DLI
- 18-24
Shouguang, Shandong, China
Monsoon Continental (Dwa)
- Summer DLI
- 42-50
- Winter DLI
- 14-20
Almería (Campo de Dalías), Spain
Hot Semi-Arid (BSh / Csa)
- Summer DLI
- 52-58
- Winter DLI
- 18-23
Salinas Valley, California, USA
Cool-Summer Mediterranean (Csb)
- Summer DLI
- 42-50
- Winter DLI
- 16-22
Buyeo (Geum River Basin), South Korea
Continental Monsoon (Dwa)
- Summer DLI
- 36-44
- Winter DLI
- 12-17
Nonsan, Chungnam, South Korea
Continental Monsoon (Dfa)
- Summer DLI
- 36-44
- Winter DLI
- 12-17
Gimje Smart Farm Valley, South Korea
Continental Monsoon (Dfa)
- Summer DLI
- 38-46
- Winter DLI
- 12-18
Miryang, Gyeongnam, South Korea
Humid Subtropical (Cfa)
- Summer DLI
- 40-48
- Winter DLI
- 14-20
Ierapetra, Crete, Greece
Warm Semi-Arid Aegean (BSh)
- Summer DLI
- 54-62
- Winter DLI
- 20-25
Santa Maria, California, USA
Mediterranean Marine (Csb)
- Summer DLI
- 45-52
- Winter DLI
- 18-24
Toyohashi, Aichi Prefecture, Japan
Humid Subtropical Pacific (Cfa)
- Summer DLI
- 40-48
- Winter DLI
- 14-19
Kochi (Tosa Bay), Japan
Humid Subtropical High Sunshine (Cfa)
- Summer DLI
- 42-50
- Winter DLI
- 16-22
Marana & Tucson, Arizona, USA
Hot Desert (BWh)
- Summer DLI
- 52-60
- Winter DLI
- 24-30
Arava Valley / Ein Yahav, Israel
Hyper-Arid Rift Valley (BWh, -100m MSL)
- Summer DLI
- 58-68
- Winter DLI
- 24-30
Souss-Massa Valley (Agadir), Morocco
Hot Semi-Arid Atlantic (BSh)
- Summer DLI
- 50-58
- Winter DLI
- 20-26
Kunming (Spring City), Yunnan, China
Subtropical Highland (Cwb, 1,900m)
- Summer DLI
- 38-46
- Winter DLI
- 22-28
Culiacán (Sinaloa Valley), Mexico
Hot Semi-Arid / Tropical Savanna (BSh)
- Summer DLI
- 50-58
- Winter DLI
- 22-28
Al-Kharj / Riyadh Oasis, Saudi Arabia
Hyper-Arid Desert (BWh)
- Summer DLI
- 60-70
- Winter DLI
- 25-30
Al Ain, Abu Dhabi, United Arab Emirates
Hyper-Arid Desert (BWh)
- Summer DLI
- 58-68
- Winter DLI
- 26-32
Querétaro (Agropark), Mexico
High-Altitude Subtropical (Cwb, 1,900m)
- Summer DLI
- 46-54
- Winter DLI
- 26-32
Đà Lạt, Central Highlands, Vietnam
Subtropical Highland (Cwb, 1,500m)
- Summer DLI
- 32-38
- Winter DLI
- 30-36
Bogotá Savanna, Colombia
Subtropical Highland (Cfb, 2,600m Equator)
- Summer DLI
- 30-36 (12h constant)
- Winter DLI
- 30-36 (12h constant)
Cameron Highlands, Pahang, Malaysia
Equatorial Mountain Rain (Af/Cfb, 1,500m)
- Summer DLI
- 28-34
- Winter DLI
- 28-34
Cayambe, Pichincha, Ecuador
Equatorial Alpine (Cfb, 2,850m Zero Latitude)
- Summer DLI
- 35-42 (Extreme UV Index)
- Winter DLI
- 35-42 (Extreme UV Index)
Lake Naivasha (Rift Valley), Kenya
Highland Equatorial (Cfb, 1,900m)
- Summer DLI
- 38-44 (12h Day)
- Winter DLI
- 38-44 (12h Day)
Guyra (New England Plateau), NSW, Australia
Temperate Highland (Cfb, 1,330m)
- Summer DLI
- 46-54
- Winter DLI
- 16-22
Stellenbosch / Boland, Western Cape, South Africa
Mediterranean Oceanic (Csb)
- Summer DLI
- 48-56
- Winter DLI
- 14-20
Adelaide Plains (Virginia), South Australia
Hot-Summer Mediterranean (Csa)
- Summer DLI
- 52-62
- Winter DLI
- 14-20
Pukekohe, Auckland Region, New Zealand
Oceanic Temperate (Cfb)
- Summer DLI
- 44-52
- Winter DLI
- 10-15
No hub matches that filter.
🌍 Comparative Agro-Climatology & CEA Engineering Methodology
Designing a commercially viable controlled environment agriculture (CEA) facility requires matching structural typology—such as high-tech Dutch Venlo glasshouses, semi-closed positive-pressure houses, or Mediterranean Parral/Raspa y Amagado polyethylene structures—to local solar radiation and psychrometric boundary conditions. This Global Ag-Climate Atlas synthesizes 40 major horticultural clusters spanning from 56.0°N in Northern Europe to 43.5°S in Oceania.
1. Solar Daily Light Integral (DLI) & Structural Transmittance
Outdoor Daily Light Integral quantifies the cumulative photosynthetically active radiation (PAR, 400–700 nm) delivered per square meter per day (mol/m²/day). Because greenhouse superstructure frames, gutters, glazing panes, and retractable screen packages intercept 22–35% of incident photons, engineers multiply outdoor DLI by the structural hemispherical transmittance coefficient ($\tau_{\text{PAR}} \approx 0.65\text{–}0.78$) to determine true canopy DLI. High-latitude maritime and continental zones (e.g., Westland at 52.0°N, Leamington at 42.1°N, Hokkaido at 43.1°N) experience winter outdoor minimums of 4–10 mol/m²/day, requiring 160–280 µmol/m²/s of high-efficacy LED assimilation lighting and double aluminum energy screens to sustain fruiting crops.
2. Psychrometric Enthalpy, Bowen Ratio & Cooling Selection
In arid and semi-arid subtropics (e.g., Almería, Culiacán, Yuma, Riyadh, Dalby), summer DLI exceeds 50–60 mol/m²/day while ambient wet-bulb depression remains large ($\Delta T_{wb} > 10\text{ °C}$). Here, evaporative pad-and-fan systems or 70–100 bar high-pressure fogging achieve high adiabatic cooling efficiency. Conversely, in humid subtropical and tropical monsoon zones (e.g., Toyohashi, Gimje, Kunming, Cameron Highlands, Dalat), elevated ambient vapor pressure limits evaporative cooling potential, necessitating tall gutter heights (6.0–7.0 m), continuous ridge buoyancy ventilation, infrared-reflective shading screens, and active mechanical dehumidification.
Curated & Verified by Inwoo Hwang — Horticultural & CEA Systems Engineer, Inwoovation Lab. Grounded in NASA POWER satellite climatology, EN 13031-1 structural design standards, and DIN V 18599 thermal energy modeling.