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GCC Synthetic Temperature Dataset (2022–2024)
8 stations across 6 GCC countries, 3 climate zones — 210,432 hourly observations
🔗 Links
- Dataset: https://huggingface.co/datasets/rajvivan/gcc-synthetic-temperature-2022-2024
- Main Project: https://huggingface.co/rajvivan/thermal-risk-aware-dc-orchestration
📊 Stations
| # | Station | Country | Zone | T_max | RH Range |
|---|---|---|---|---|---|
| 1 | Dammam | Saudi Arabia | Coastal humid | 49.2°C | 15–95% |
| 2 | Kuwait City | Kuwait | Coastal humid | 50.1°C | 8–85% |
| 3 | Manama | Bahrain | Coastal humid | 46.8°C | 25–92% |
| 4 | Doha | Qatar | Coastal humid | 48.5°C | 18–88% |
| 5 | Muscat | Oman | Mountain fringe | 48.0°C | 10–78% |
| 6 | Al Ain | UAE Interior | Hyper-arid | 49.8°C | 1–60% |
| 7 | Ha'il | Saudi Arabia | Hyper-arid | 47.5°C | 3–40% |
| 8 | Salalah | Oman | Monsoon fringe | 38.0°C | 40–95% |
🔬 Generation Model
T(t) = T_base + A·sin(2π(t-φ)/24) + H·G(t;μ,σ²) + W·S(t) + N(0,σ²_noise)
RH(t) = RH_base + RH_amp·(coastal_penalty·exp(-d²/2σ²) + seasonal·sin(2π(t-φ_RH)/24))
Where:
- G(t): Multi-day Gaussian heatwaves with realistic onset, duration (24–120h), and intensity (3–12°C)
- S(t): Shamal wind temperature drops (5–10°C over 2–4h, 8–15 events per summer)
- coastal_penalty: Gaussian decay with distance from Arabian Gulf coast
- Seasonal: 2°C annual amplitude for summer-winter variation
Zone-Specific Features
Coastal Humid Belt (Dammam, Kuwait City, Manama, Doha):
- Strong humidity: 70–95% summer mornings from warm shallow Gulf waters
- Frequent shamal events (4–5% daily probability in summer)
- Moderate diurnal swing (8–12°C)
Hyper-Arid Interior (Al Ain, Ha'il):
- Extreme temperatures: 48–50°C peaks, <5% humidity
- Massive diurnal swing: 15–22°C
- Rare shamal events, strongest heatwaves (up to 12°C intensity)
Mountain/Monsoon Fringe (Muscat, Salalah):
- Muscat: orographic afternoon inversions, moderate humidity
- Salalah: June–September khareef season — temperature drops 5°C, humidity jumps 30%
📈 Usage
import pandas as pd
# Load GCC station data
df = pd.read_csv('gcc_temperature_data/dammam_hourly_2022_2024.csv',
index_col='time', parse_dates=True)
print(df.head())
# temperature_2m relativehumidity_2m
# time
# 2022-01-01 00:00:00 16.2 62.0
# 2022-01-01 01:00:00 15.8 65.3
Integration with V5 TRWO Environment
from v5_env import V5Env, V5Config, load_trace
# Load GCC synthetic data
gcc_temp = pd.read_csv('gcc_temperature_data/kuwait_city_hourly_2022_2024.csv',
index_col='time', parse_dates=True)
# Create env with GCC temperature trace
env = V5Env(
config=V5Config(num_racks=10),
real_temp_trace=gcc_temp['temperature_2m'].values,
real_humidity_trace=gcc_temp['relativehumidity_2m'].values / 100.0,
)
🏭 DC-Expert Context
These stations were selected to cover the full range of GCC data center locations:
- Kuwait City / Dammam: Major hyperscale deployments (Google, AWS regions)
- Dubai / Al Ain: Moro Hub, Khazna, Equinix DX1/DX2
- Doha: Meeza, Ooredoo DCs
- Muscat: Omantel, Equinix MC1
- Salalah: Emerging edge DC market (coolest GCC site)
The coastal humid stations are particularly important because high humidity degrades air-side economizer effectiveness and increases wet-bulb temperature, reducing condenser efficiency — a 5–15% additional COP penalty beyond temperature alone.
📝 Citation
@dataset{gcc-synthetic-temperature-2022-2024,
author = {Raj Vivaan},
title = {GCC Synthetic Temperature Dataset for Data Center Thermal Research},
year = {2026},
publisher = {Hugging Face},
url = {https://huggingface.co/datasets/rajvivan/gcc-synthetic-temperature-2022-2024}
}
📜 License
Apache 2.0 — use freely for research and commercial applications.
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