reprinted July 2014 surface temperature inversions and spraying FACT SHEET NORTHERN, SOUTHERN AND WESTERN REGIOns THe infLuenCe Of SurfACe TemPerature inverSiOnS On SPrAy OPeratiOnS in cooling night conditions airborne pesticides can concentrate near the surface and unpredictable winds can move droplets away from the target. understanding weather conditions can help spray applicators avoid spray drift. warm air Key points cool air Where surface temperature inversion conditions exist it is unsafe for Top of the inversion spraying due to the potential for spray drift. Spray applied at dawn, dusk and Height during the night is likely to be affected by a surface temperature Night profile inversion. Day profile During surface temperature inversions, air near the ground lacks turbulence. This can lead to airborne pesticides remaining at high concentrations in the air at or near cool warm the surface. Temperature The direction and distance that pesticides can move in the air close FIGURE 1 Typical vertical temperature profiles for a point in time to the ground is very hard to predict during the night and day. At low levels, the day profile typically cools when surface inversions exist. with height and the night profile typically warms with height. Little change occurs at elevated altitudes. SOurCe GrAeme TePPer During daylight hours the temperature of airborne droplets and helps to drive many of When this occurs close to the ground it is the soil surface gradually increases. Air in them back towards the ground. called a surface temperature inversion. contact with the ground also warms (figure When this dilution occurs, a safe buffer in a surface temperature inversion 1). in this situation the air temperature distance between the sprayed area and the point where the temperature stops normally becomes cooler with height. potentially sensitive areas downwind from increasing and begins to decrease is the top Wind speeds during daylight hours will the application site can be estimated. of the inversion layer. generally be more than 3 to 4km/h and the surface temperature When a strong surface temperature air movement across the surface will tend to inversions inversion has established, it can act like be turbulent. a barrier, isolating the inversion layer from inversion conditions can differ significantly the normal weather situation, especially the Turbulence close to the ground causes the from the broader forecast weather patterns. air to mix, due to the rolling motion of the normal wind speed and direction (figure 2). During the night the ground loses heat and air across the ground surface. mixing is also the low-level air cools (figure 1). This results Surface temperature inversion conditions are caused by thermals, which interrupt airflow. in air temperature increasing with height and unsafe for spraying as the potential for spray This mixing of the air assists in diluting the temperature profile is said to be inverted. drift is high. Level 1, Tourism House | 40 Blackall Street, Barton ACT 2600 | PO Box 5367, Kingston ACT 2604 | t +61 2 6166 4500 | f +61 2 6166 4599 | e [email protected] | W www.grdc.com.au Page 2 warm air typical wind profile inversion wind profile cool air longer arrow equals greater wind strength Height Inversion layer Calm or light winds so long as local winds warming land cooling land do not develop FIGURE 2 Air movement under a surface temperature inversion differs from a typical wind profile (left). Surface winds de-couple from the surface, accelerate and flow over the inversion. Within the inversion, winds are typically light and often drain down slope, regardless of the overlying wind direction. Under an inversion the shape of the landscape also influences the direction in which airborne droplets will move (right). SOurCe GrAeme TePPer under a surface temperature inversion: research supported by the GrDC is to the ground to become cooler than further investigating the development and the air above. The three main reasons air movement is much less turbulent so experienced in broadacre agriculture are: the air does not mix in the same way as implications of temperature inversions in relation to spray application. during the day; 1. radiation inversions (created airborne droplets can remain When and why do surface by radiation cooling) concentrated in the inversion layer for temperature inversions long periods of time; radiation inversions can form at any time occur? during the night when wind speed is less the direction and distance pesticides than about 11km/h and cloud cover does movement is very hard to predict; Surface temperature inversions usually not severely restrict surface cooling. in develop overnight and can persist well into the movement of airborne droplets will calm and clear sky conditions they may the next day. vary depending on the landscape; and form just before sunset. Once the sun has droplets or their remnants can move in They can result from a number of set and has stopped heating the ground, different ways (figure 3). processes that cause the air closest heat radiates back into space, causing the Pho T o: BILL G o RD o N Under a surface temperature inversion air can separate into very stable layers (laminates) that can concentrate and transport airborne pesticides. Page 3 ground to cool. in turn, the air in contact 3. inversions created by smoke or dust hangs in the air and with the ground becomes cooler than the vegetation moves sideways, just above the air higher in the atmosphere. This generates surface; and vegetation and crops can shade the the surface temperature inversion. cumulus clouds that have built up during ground underneath them. The air in the day collapse towards evening. radiation inversions are the most contact with the ground will stay cooler dangerous for spraying operations as than adjacent areas where there is less other clues they cause airborne droplets to remain groundcover. This often occurs just concentrated at a low level for long periods. after sunrise. The air moving above the A surface temperature inversion is likely to Winds within the inversion can carry these vegetation or crop may be warmer than be present if: droplets long distances. the air below the vegetation. This can allow wind speed is constantly less than On gentle slopes, concentrated droplets airborne droplets to travel over, rather than 11km/h in the evening and overnight; can be transported many kilometres by through, vegetation. cool, off-slope breezes develop during drainage winds towards the lowest point in Transpiration from a dense crop canopy the evening or overnight; the catchment. under an inversion, where on a hot day can form a cool layer of air distant sounds become clearer and water runs from a property, droplets can just above the crop. Later in the day (when easier to hear; and move. See figure 3 (c). wind speeds tend to reduce) this layer of aromas become more distinct during cooler air can act like an inversion over the the evening than during the day. 2. inversions created by crop, making penetration of smaller spray advection (cool or warm air droplets into the canopy very difficult and clues that a surface movement) increasing the risk of off-target movement. temperature inversion is unlikely Cooler, denser air can move into an area and slide under layers of less dense, recognising a surface Applicators should always expect that a warm air. temperature inversion surface temperature inversion is most likely to have formed at sunset and will persist for This can happen when a cold front moves The scientific method for detecting a sometime after sunrise. However, a surface into an area, or a sea breeze pushes surface temperature inversion requires temperature inversion is unlikely if one or cooler air inland. it can also happen when the accurate measurement of the air more of the following has occurred: denser cool air moves down a slope temperature close to the ground and at and slides underneath layers of warm a height of at least 10m. On-farm, this continuous overcast weather, with low air in lower parts of the catchment. if is usually not practical, so most spray and heavy cloud; applicators must rely on visual clues. this occurs, the intensity of a radiation continuous rain; inversion increases. visual clues wind speed remains above 11km/h for Warm air can move over cool surfaces; the whole* time between sunset A surface temperature inversion is likely to some of the air closest to the ground and sunrise; and be present if: becomes cooler while the higher air stays after a clear night, cumulus clouds warmer. mist, fog, dew or a frost have occurred; begin to form. A A Droplets travel many kilometres close to the surface due to light breezes that lack turbulence, so the air is not mixed. Light winds B B Airborne pesticides and water vapour can move down gentle slopes and concentrate in lower parts of Drainage winds the catchment. C C Caught in complex thermals, droplets can move in Light winds unpredictable directions, particularly when the surface Base of eroding inversion temperature inversion begins to break down as the sun begins to heat the ground. At this time droplets can be lifted into higher layers of the inversion, where the Thermals Light winds wind movement could be in a different direction to that experienced closer to the ground. Legend Fine droplets, particles and vapour Medium droplets Coarse droplets FIGURE 3 Possible movement of airborne droplets in surface temperature inversion conditions. SOurCe GrAeme TePPer Page 4 *Sometimes the overnight wind speed Be aware of sensitive areas around the will provide efficacy. every nozzle can can pick up from virtually calm to speeds area to be sprayed. Sensitive areas produce small, driftable droplets. using greater than 11km/h during a surface include lower points in the catchment coarser spray qualities reduces the temperature inversion.