Weather and Plant Diseases
We all know how weather affects plant diseases: Warm, moist conditions are perfect for the growth of plant pathogens. But that’s not what this article is about. This article is about how plant pathogens can affect the weather.
But before we get into that, we need a little background information on the chemistry of how ice forms. (Trust me on this one.) Most people consider 32°F to be the freezing point of water, and generally speaking, this is true. Technically, however, 32°F is considered to be the melting point of water. This is because pure water, really pure water, often experiences supercooling; not freezing until it reaches temperatures as low as -40°F. This is because at temperatures just below 32°F more than 100,000 water molecules need to latch together before an ice crystal becomes stable enough to grow on its own. The chances of this many molecules randomly coming together to form an ice crystal are exceedingly low, even at colder temperatures. In our everyday world of puddles, ponds, and ice cube trays, tiny particles of dust and such act as a template for the hexagonal lattice of an ice crystal to form on, triggering ice formation at 32°F. This process is called “ice nucleation.”
Climatologists have been aware of this for decades. They have long assumed that tiny dust particles blown up from the earth’s surface into the atmosphere induce ice crystal formation in clouds, triggering precipitation. (Only ice crystals grow fast enough to reach the critical mass necessary to fall from the cloud as rain or snow.) But they have never been able to identify which of the many types of dust particles have the right surface chemistry to act as the ice crystal template.
Enter Pseudomonas syringae. P. syringae is a bacterium that causes disease in a wide variety of plants. It also produces proteins on its surface that make it act as a “biological ice nucleator,” triggering frost formation resulting in injury to plants.
Ice crystals forming on the plant rupture the cells, making the nutrients within available to the bacteria. P. syringae, along with a host of other bacteria, fungal spores and algae, get blown up into the atmosphere along with all that dust that
climatologists have been studying, and may be the true source of ice crystal
formation in clouds.
Is this just happenstance, or is it an evolutionary strategy? Are bacteria rising into the atmosphere to trigger rain to produce more plants to feed on?
Are forests making more rain by releasing bacteria into the atmosphere?
And what about us? How can we exploit this extraordinary characteristic of an organism we have long considered a “pest?” The Biosciences Division of the U. S.
Department of Energy has supported considerable work on P. syringae. There is promise in its use in freezing foods. It has been used in the production of artificial snow for skiing and artificial ice for skating rinks. It has also been used to create
artificial ice islands in cold oceans to facilitate oil drilling, and research is being conducted in using it to produce mountains of artificial snow to use for summer cooling.
So, while I hate to see Pseudomonas blight on my lilacs, the more I learn, the more I realize that nothing in nature is all bad.






This six-foot diameter Incense Cedar is a good example!

