All Meteorology Calculators Related Post

Droplet Growth Calculator About the Droplet Growth Calculator The Droplet Growth Calculator is a scientifically accurate, real-time online tool that computes the diffusional (condensational) growth rate of cloud droplets and ice crystals using the classic Maxwellian diffusion theory with ventilation and kinetic corrections. It implements the full Pruppacher & Klett (2010) formulation including curvature (Kelvin) […]

Cloud Microphysics Calculator About the Cloud Microphysics Calculator The Cloud Microphysics Calculator is a comprehensive, scientifically accurate online tool that performs key calculations in cloud microphysics, including droplet activation, diffusional growth, collision-coalescence time, ice crystal growth rate, rime accretion, terminal velocity, and precipitation efficiency. It implements peer-reviewed parameterizations from Pruppacher & Klett (2010), Rogers &

Collision-Coalescence Calculator About the Collision-Coalescence Calculator The Collision-Coalescence Calculator is a scientifically accurate, real-time online tool that estimates the time required for precipitation formation in warm clouds through the collision-coalescence process — the dominant mechanism for raindrop growth in clouds with temperatures above 0 °C. It implements the continuous collection model of Berry & Reinhardt

Cold Cloud Precipitation Calculator About the Cold Cloud Precipitation Calculator The Cold Cloud Precipitation Calculator is a scientifically accurate, real-time online tool that estimates the time required for precipitation formation in cold clouds (containing ice) through the Bergeron-Findeisen (ice crystal) process and riming (accretion). It implements the classic diffusion-deposition growth model for ice crystals and

Warm Cloud Precipitation Calculator About the Warm Cloud Precipitation Calculator The Warm Cloud Precipitation Calculator is a scientifically rigorous, real-time online tool designed for meteorologists, cloud physicists, and agricultural researchers to estimate the time required for precipitation formation in warm clouds (T > 0 °C) through the collision-coalescence process. It implements the continuous collection model

Lidar Ratio Calculator About the Lidar Ratio Calculator The Lidar Ratio Calculator is an essential online tool for atmospheric scientists, lidar operators, and researchers to determine or estimate the lidar ratio (extinction-to-backscatter ratio, S_a in steradians, sr) — a critical parameter in elastic-backscatter lidar retrievals of aerosol extinction profiles. This calculator provides standard, peer-reviewed typical

Saffir-Simpson Scale Calculator About the Saffir-Simpson Scale Calculator The Saffir-Simpson Scale Calculator is a scientifically accurate, real-time online tool that instantly determines the official Saffir-Simpson Hurricane Wind Scale category (1–5) based on sustained wind speed, and provides detailed expected damage, storm surge, and impacts according to the National Hurricane Center (NHC/NOAA) standards. Developed by Herbert

Beaufort Scale Calculator About the Beaufort Scale Calculator The Beaufort Scale Calculator is a scientifically accurate, real-time online tool that instantly determines the Beaufort wind force number (0–12) and corresponding description from observed wind speed or visible sea/land effects. It strictly follows the official Beaufort scale as defined by the World Meteorological Organization (WMO) and

Latent Heat Flux Calculator About the Latent Heat Flux Calculator The Latent Heat Flux Calculator is a scientifically accurate, real-time online tool that computes latent heat flux (LE or λET) — the energy used for evapotranspiration from soil, plants, and water surfaces — using the bulk aerodynamic formula, Penman-Monteith equation, Bowen ratio method, and eddy

Sensible Heat Flux Calculator About the Sensible Heat Flux Calculator The Sensible Heat Flux Calculator is a scientifically accurate, real-time online tool that computes sensible heat flux (H) — the turbulent transfer of heat between the Earth’s surface and the atmosphere due to temperature differences — using the bulk aerodynamic formula, eddy covariance method, and