Humidity is a critical factor in cannabis cultivation, one that is much discussed but also often misunderstood. It’s about time we set the facts straight.

We want to help you keep your buds dry and healthy, so this may be a bit long winded. Take a deep breath, but don’t sweat.

WHAT IS HUMIDITY?

Air is comprised of many different gases, one of which is water vapor- the gaseous form of water. The amount of water vapor in the air is measured by relative humidity (RH). This is basically the amount of water vapor in the air, as a percentage of the amount of water the air can contain.

RH is determined by two factors- the amount of water vapor and the air temperature. With this in mind, we can understand the importance of relative humidity in a growing facility.

WHY DO WE NEED TO MAINTAIN A CERTAIN RELATIVE HUMIDITY LEVEL?

Humidity is a major factor in the cannabis industry due to the dreaded Botrytis, a moisture-loving fungus, most commonly known as “bud rot”.

Humidity control equals bud rot prevention. That’s the bottom line.

Due to the dense nature of the cannabis bud, it’s highly susceptible to humidity build up. This is caused by the plant continuously emitting water vapor through its leaves. this is intensified in cannabis, because the bud itself contains leaves, known as “sugar leaves”. Because the bud is dense, this humidity gets trapped.

Humidity is water vapor in the air, but the real enemy is actual liquid water. Water tends to condense on cold surfaces. And this is the tricky part, the plant itself may be the cold surface! Plants transpire as they cool themselves off, sort of like sweat, which renders them colder than their immediate environment. With cannabis, the humidity, which is created inside the dense bud, condenses on the cold surfaces, also inside the bud. This is great for mold and a major concern for growers.

To better understand the relationship between humidity and air temperature, we should have a look at the dew point.

DEW POINT – THE KEY TO CONDENSATION PREVENTION

The dew point is the point at which air becomes saturated with water vapor, forcing the water to condense from a gas form into liquid. Basically, it’s the point at which temperature has dropped enough to force water to appear.

This may not be intuitive, as water vapor is invisible, so we’ll use an everyday life example. Following is the Psychometric table:

psychrometric chart

When you pour a cold drink into a glass, you’ll notice water forming on the outside. This happens because the cold drink lowers the temperature of the glass, pushing it beyond the dew point. The water vapor from the surrounding air condenses onto the outside surface of the glass and that’s where you get the formation of water droplets.

This is the basic concept. The dew point is the temperature at which humidity turns into water.

HOW IT WORKS

Temperature and relative humidity are intertwined. It’s easy to think of air as a sponge in this scenario; it contains water up to a certain point and once it is full, water begins to appear. If the temperature is constant, we can reduce the relative humidity by removing water vapor from the air. This would stop the appearance of water.

But when temperature changes, relative humidity levels will also change. Hotter air can contain more water than colder air. When temperatures rise, relative humidity drops, reducing condensation.

Water condensation can be managed and prevented through control of humidity and temperatures, such as with DryGair’s dehumidification systems. This is the important part- the dew point is basically a breakdown of this relationship.

The following graph represents the dew point as a function of RH at a given air temperature:

dew point temperature

dew point as a function of RH at a given air temperature

Graph of Dewpoint vs. Air Temperature at 70% Relative Humidity. Based on the Magnus-Tetens approximation.

 

This graph represents 70% RH. You can notice that at an air temperature of 70°F (bottom axis), the graph aligns with 60°F dew point temperature (left axis). This means that if your greenhouse air is currently at 70% relative humidity at 70°F, you can go as low as 60°F before liquid water begins to appear. If any one surface in the growing facility reaches 60°F or below, water will condense on it. Cooler surfaces are typically ceilings and walls, which have greater contact with the outdoors, as well as metal pipes and railings, or as we mentioned earlier, the plants themselves.

A SMARTER APPROACH – THE DRYGAIR SOLUTION

A combined approach, based on knowledge, allows us to do the minimum. We don’t mean minimum care, we mean minimum cost. The DryGair Solution

Understanding what the dew point is and the factors that affect it provides us a better understanding of what’s really going on in our operation. What really happens when we heat up, or allow the air to cool down. It’s not just about temperature, it’s about humidity as well and the dew point encapsulates this.