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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.

52.0°N

Bleiswijk, Netherlands

Maritime Temperate (Cfb)

Summer DLI
34-40
Winter DLI
6-9
52.0°N

Naaldwijk (Westland East), Netherlands

Maritime Temperate (Cfb)

Summer DLI
35-41
Winter DLI
6-10
52.0°N

Westland, Netherlands

Maritime Temperate (Cfb)

Summer DLI
38-42
Winter DLI
5.4-8.5
51.4°N

Straelen / Lower Rhine, Germany

Continental Transition (Cfb)

Summer DLI
36-42
Winter DLI
5-9
49.5°N

Nürnberg / Knoblauchsland, Bavaria

Warm-Summer Humid (Cfb)

Summer DLI
38-45
Winter DLI
7.2-10.5
49.1°N

Delta / Fraser Valley, BC, Canada

Pacific Maritime (Cfb)

Summer DLI
36-44
Winter DLI
6-11
48.4°N

Brittany (Finistère), France

Hyper-Maritime Cool Summer (Cfb)

Summer DLI
32-38
Winter DLI
7-11
42.0°N

Leamington / Kingsville, Ontario, Canada

Humid Continental (Dfa)

Summer DLI
40-48
Winter DLI
8-14
38.2°N

Morehead (Appalachian Basin), Kentucky, USA

Humid Subtropical (Cfa)

Summer DLI
38-46
Winter DLI
10-16
38.0°N

Murcia (Campo de Cartagena), Spain

Semi-Arid Mediterranean (BSk)

Summer DLI
48-56
Winter DLI
15-20
36.9°N

Antalya (Aksu & Kumluca), Turkey

Mediterranean Hot Summer (Csa)

Summer DLI
50-58
Winter DLI
16-22
36.9°N

Ragusa / Vittoria, Sicily, Italy

Hot Mediterranean (Csa)

Summer DLI
52-60
Winter DLI
18-24
36.9°N

Shouguang, Shandong, China

Monsoon Continental (Dwa)

Summer DLI
42-50
Winter DLI
14-20
36.8°N

Almería (Campo de Dalías), Spain

Hot Semi-Arid (BSh / Csa)

Summer DLI
52-58
Winter DLI
18-23
36.7°N

Salinas Valley, California, USA

Cool-Summer Mediterranean (Csb)

Summer DLI
42-50
Winter DLI
16-22
36.2°N

Buyeo (Geum River Basin), South Korea

Continental Monsoon (Dwa)

Summer DLI
36-44
Winter DLI
12-17
36.2°N

Nonsan, Chungnam, South Korea

Continental Monsoon (Dfa)

Summer DLI
36-44
Winter DLI
12-17
35.8°N

Gimje Smart Farm Valley, South Korea

Continental Monsoon (Dfa)

Summer DLI
38-46
Winter DLI
12-18
35.5°N

Miryang, Gyeongnam, South Korea

Humid Subtropical (Cfa)

Summer DLI
40-48
Winter DLI
14-20
35.0°N

Ierapetra, Crete, Greece

Warm Semi-Arid Aegean (BSh)

Summer DLI
54-62
Winter DLI
20-25
34.9°N

Santa Maria, California, USA

Mediterranean Marine (Csb)

Summer DLI
45-52
Winter DLI
18-24
34.8°N

Toyohashi, Aichi Prefecture, Japan

Humid Subtropical Pacific (Cfa)

Summer DLI
40-48
Winter DLI
14-19
33.6°N

Kochi (Tosa Bay), Japan

Humid Subtropical High Sunshine (Cfa)

Summer DLI
42-50
Winter DLI
16-22
32.4°N

Marana & Tucson, Arizona, USA

Hot Desert (BWh)

Summer DLI
52-60
Winter DLI
24-30
30.5°N

Arava Valley / Ein Yahav, Israel

Hyper-Arid Rift Valley (BWh, -100m MSL)

Summer DLI
58-68
Winter DLI
24-30
30.4°N

Souss-Massa Valley (Agadir), Morocco

Hot Semi-Arid Atlantic (BSh)

Summer DLI
50-58
Winter DLI
20-26
25.0°N

Kunming (Spring City), Yunnan, China

Subtropical Highland (Cwb, 1,900m)

Summer DLI
38-46
Winter DLI
22-28
24.8°N

Culiacán (Sinaloa Valley), Mexico

Hot Semi-Arid / Tropical Savanna (BSh)

Summer DLI
50-58
Winter DLI
22-28
24.7°N

Al-Kharj / Riyadh Oasis, Saudi Arabia

Hyper-Arid Desert (BWh)

Summer DLI
60-70
Winter DLI
25-30
24.2°N

Al Ain, Abu Dhabi, United Arab Emirates

Hyper-Arid Desert (BWh)

Summer DLI
58-68
Winter DLI
26-32
20.6°N

Querétaro (Agropark), Mexico

High-Altitude Subtropical (Cwb, 1,900m)

Summer DLI
46-54
Winter DLI
26-32
11.9°N

Đà Lạt, Central Highlands, Vietnam

Subtropical Highland (Cwb, 1,500m)

Summer DLI
32-38
Winter DLI
30-36
4.7°N

Bogotá Savanna, Colombia

Subtropical Highland (Cfb, 2,600m Equator)

Summer DLI
30-36 (12h constant)
Winter DLI
30-36 (12h constant)
4.5°N

Cameron Highlands, Pahang, Malaysia

Equatorial Mountain Rain (Af/Cfb, 1,500m)

Summer DLI
28-34
Winter DLI
28-34
0.0°N

Cayambe, Pichincha, Ecuador

Equatorial Alpine (Cfb, 2,850m Zero Latitude)

Summer DLI
35-42 (Extreme UV Index)
Winter DLI
35-42 (Extreme UV Index)
0.7°S

Lake Naivasha (Rift Valley), Kenya

Highland Equatorial (Cfb, 1,900m)

Summer DLI
38-44 (12h Day)
Winter DLI
38-44 (12h Day)
30.2°S

Guyra (New England Plateau), NSW, Australia

Temperate Highland (Cfb, 1,330m)

Summer DLI
46-54
Winter DLI
16-22
33.9°S

Stellenbosch / Boland, Western Cape, South Africa

Mediterranean Oceanic (Csb)

Summer DLI
48-56
Winter DLI
14-20
34.7°S

Adelaide Plains (Virginia), South Australia

Hot-Summer Mediterranean (Csa)

Summer DLI
52-62
Winter DLI
14-20
37.2°S

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.