Understanding Cloud Seeding: Australia’s Approach to Artificial Rainfall
Water security is a perennial challenge for Australia, leading to decades of experimentation with weather modification. While the idea of “artificial mountains” to force rainfall is not supported by current data, Australia has a long history of employing cloud seeding—a scientific process designed to stimulate precipitation in specific atmospheric conditions.
- Cloud seeding uses substances like silver iodide or dry ice to encourage rain or snow.
- It requires existing rain-bearing clouds to work; it cannot create rain during a drought.
- Australia has conducted trials since the 1940s, primarily in high-level mountainous regions.
- Recent active programs have been managed by entities such as Snowy Hydro and Hydro Tasmania.
What is Cloud Seeding and How Does it Work?
Cloud seeding is a type of weather modification that aims to change the amount or type of precipitation, disperse fog, or mitigate hail. The process involves dispersing substances into the air that act as cloud condensation or ice nuclei. These “seeds” provide a surface for moisture to cling to, accelerating the formation of raindrops or snowflakes.
Common Seeding Agents
Depending on the goal and the cloud type, different materials are used:
- Silver Iodide: Commonly used in “glaciogenic” seeding to convert super-cooled liquid water into ice crystals.
- Dry Ice: Used to cool clouds and stimulate precipitation.
- Hygroscopic Materials: Substances like table salt are used to attract moisture in specific cloud environments.
- Potassium Iodide: Another agent used to serve as a nucleus for condensation.
Delivery Methods
These agents are introduced into the atmosphere via two primary methods: ground-based generators (emitters) and aircraft that dump substances directly into the clouds.
Cloud Seeding in Australia: A Historical Perspective
Australia’s journey with weather modification began in the 1940s. The CSIRO led early research, including dropping dry ice into cumulus clouds in the late 1940s and early 1950s. By the mid-1950s, trials expanded to South Australia and Queensland using both airborne and ground-based silver iodide generators.
Between 1955 and 1963, intensive experiments were conducted in several key regions, including the Snowy Mountains, the Novel England region of NSW, and the Yorke Peninsula in South Australia.
Effectiveness and Limitations
Cloud seeding is not a universal solution for water scarcity. Its success depends heavily on geography and existing weather patterns.
The Role of Geography
Successful operations typically require high-level mountainous regions. In Australia, experimental trials in lower-lying areas have failed to validate the technique’s value for rain enhancement.
The Drought Paradox
A critical limitation of cloud seeding is that it cannot generate rain during a drought. Because the process requires the presence of rain-bearing clouds to work, it is ineffective when the atmosphere is completely dry.
Case Study: Tasmania
The debate over efficacy continues. In 2016, Hydro Tasmania conducted seeding operations prior to significant flooding in north-western Tasmania. Yet, an independent report later concluded that the seeding had “no measurable impact on precipitation.”
Current Status of Operations
While many early CSIRO trials ended in the late 1980s, active programs persisted in mountainous areas for several more decades. Snowy Hydro in New South Wales operated cloud seeding programs until 2023, and Hydro Tasmania conducted operations until 2016.
Frequently Asked Questions
Does cloud seeding cause floods?
While some community backlash occurred following floods in Tasmania in 2016, independent expert reviews found that the cloud seeding performed by Hydro Tasmania had no measurable impact on the precipitation levels.

Is cloud seeding safe?
The process involves introducing “chemically inert” seeds or crystals into the atmosphere to encourage the formation of ice crystals.
Can it be used anywhere in Australia?
No. It is most effective in cold-weather mountainous areas. Trials in lower-lying regions have generally been unsuccessful.
Related reading