Swamp Cooler Temperature Calculator

Swamp Cooler Temperature Calculator

Estimate wet-bulb temperature, wet-bulb depression, relative humidity, evaporative saturation effectiveness, leaving air temperature, room temperature drop, and climate suitability for an evaporative cooler.

🏜Climate presets

Temperature and cooler inputs

Enter outdoor dry-bulb conditions and cooler details. The calculator estimates wet-bulb with the Stull approximation, backs into vapor pressure and relative humidity, then applies saturation effectiveness to predict supply air.

Values convert internally for the psychrometric formulas.
Shaded outdoor air temperature entering the pads.
Use afternoon RH if sizing for peak heat.
Typical direct coolers run about 65% to 85% when pads and airflow are right.
Used to estimate practical indoor temperature drop.
The score compares predicted stabilized indoor air to this target.
Room or home area served by this cooler.
Volume helps rate airflow intensity.
Use delivered airflow through wet pads, not just catalog maximum.
Open windows, relief vents, or doors that allow supply air to escape.
High gains reduce the realized room temperature drop.
Check the inputs. Temperatures, humidity, effectiveness, airflow, area, height, and exhaust area must be in practical ranges.
Leaving Air Temperature
0
supply air estimate
Wet-Bulb Depression
0
dry bulb minus wet bulb
Indoor Temperature Drop
0
stabilized room estimate
Suitability Score
0
climate and setup fit

Calculation breakdown

📊Evaporative cooler spec grid

78%
Saturation effectiveness
4500
Cooler airflow CFM
2.0
Sq ft vent per kCFM
28
Air changes per hour

📋Reference tables

Climate band Outdoor RH Typical wet-bulb depression Cooling outlook
Excellent desert10% to 25%25°F to 38°FStrong leaving-air drop
Good dry inland25% to 35%18°F to 28°FUseful whole-room cooling
Borderline plains35% to 45%12°F to 20°FWorks best during driest hours
Weak humid heat45% to 55%7°F to 14°FSmall comfort benefit
Poor humid climateAbove 55%Under 10°FOften not suitable indoors
Cooler type Typical effectiveness Airflow range Temperature use case
Portable direct unit55% to 68%250 to 1200 CFMSpot cooling in dry rooms
Window side-discharge68% to 78%1800 to 4500 CFMRoom or small-home cooling
Rooftop whole-house72% to 85%3500 to 7500 CFMDry-climate whole-home cooling
Ducted direct cooler65% to 80%3000 to 8000 CFMDistributed supply with duct losses
Indirect/direct two-stage85% to 95%1200 to 6000 CFMLower supply temp with less moisture
Greenhouse pad wall70% to 88%Large fan bankHigh airflow through wetted media
Input or formula Calculator role Core equation Result meaning
Dry-bulb temperatureOutdoor heat inputMeasured shade airUpper limit before evaporation
Wet-bulb temperatureEvaporation limitStull RH approximationLowest direct evaporative target
Wet-bulb depressionCooling potentialDry bulb minus wet bulbMaximum direct cooling gap
Saturation effectivenessCooler performanceSupply = dry - depression x effectivenessPredicted leaving air
Suitability scoreClimate fitRH, drop, vent, airflow, target blendQuick practical rating
Preset example Dry bulb and RH Supply estimate Suitability
Phoenix Afternoon100°F, 18%73°FExcellent

💡Swamp cooler temperature tips

Judge the cooler by wet-bulb depression.

Dry air creates a large gap between dry-bulb and wet-bulb temperature. The cooler can only use a percentage of that gap, so pad condition and airflow matter.

Exhaust area protects real performance.

Direct evaporative coolers need relief air. If windows or vents are too tight, airflow falls and indoor humidity rises faster than the temperature drops.

In humid conditions, your swamp cooler is going to work or not based off how much moisture the air can actualy absorb before it gets saturated. If you know the right numbers, you can see what’s happening, it’s predictable physics. Before fully saturated, what does the air do with water? What happens when it won’t take any more? No matter how thick a pad or powerful a fan, there is no forcing evaporation.

After plugging in your humidity and local temperature into the calculator above, it’ll do all that psychrometric work for you. No more guesswork on what’s too much or not enough humidity on a hot day. It calculates something called wet-bulb depression, how far below your current air temp you can get the air by evaporative cooling. That is your comfort potential. The closer the number gets to zero (meaning lots of moisture in the air), the less your supply air will be able to cool down. This is a little math fact with a huge impact on your summer strategy.

How Humidity Changes Your Swamp Cooler’s Power

The effectiveness of saturation is another bit of tech-speak that most homeowners gloss over. This section of inputs shouldn’t be skipped though. In reality, no real-world evaporative cooler operate at peak efficiency. If your pads are dirty they restrict air flow and won’t allow for even evaporation across the pad surface. An unused cooler could barely manage 60% effectiveness whereas a brand-new one might get up to 80%. This variable change the calculator’s predicted leaving air temp so you can see how things will shake out given your current conditions versus a perfect standard. It sets you up for a realistic expectation, not a best case.

Airflow is another thing that trips up users’ intuitions. More air = cooler room, right? Not so fast. Trapped heat is a fact of life. Direct evaporative coolers relies on relief vents or open windows to expel humid air while drawing in drier supply air. Pressure rises within your house if there’s no place for the displaced volume to go, stalling all airflow. The tool calculates how many times the air in your room should be replaced each hour by looking at both floor area and ceiling height.

Is the relief opening too small compared to size of your fan? What you’ll feel isn’t cooling, it’s humidity. That’s what most people miss when they seal every window shut, figuring they’re preserving the cool air. In reality, they’re choking the system.

That said, even within very short distances, regional climate ranges is quite different. In desert climates, starting humidity levels are low and there’s plenty of space for cool-down by evaporation. In humid plains climates, while the outside temps may be high, the margin is much narrower and evaporative cooling won’t do much for your comfort level. The page’s reference table maps out those bands neatly so you can locate yours. This helps you understand why it makes sense (or not) to go big with your roof unit. Or, you might just have to face it: sometimes you need an air conditioner after all.

While size matter initially, longer term maintenance is more important. Scale build-up restricts water flow and creates dry areas on the pads which receive no cooling whatsoever. Before maximum heat arrives, flush the system so you’re still effective at getting them good and wet when needed most. Early season checks of exhaust ventilation paths are also helpful as dust clogged screens or sticky doors will kill your airflow rate without even hinting at what’s going wrong.

Ultimately, it’s all about working within the atmospheric conditions. On a sweltering, sunny and dry day, an evaporative cooling system cools the air and creates a nice, refreshing breeze that feels much cooler then what the thermometer registers. During humid days, it just circulates moist air, which isn’t going to help. So understanding the capabilities of your equipment and your environment will help you manage realistic expectations during those hot summer months. Instead of trying to figure out why the temperature isn’t falling as low as you’d like, you can learn how to dial in the right setting. This helps you get the best results possible given current conditions.

Swamp Cooler Temperature Calculator

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