Simulation modeling of the effects of short and long-term climatic variations on carbon balance of apple trees A. N. Lakso1, M.D. White2 and D. S. Tustin2 1 2 Dept. of Horticultural Sciences, NY State Agricultural Experiment Station, Geneva, NY 14456, USA HortResearch, Private Bag 1401, Havelock North, New Zealand Abstract Effects of short- and long-term climatic variation and foliar pests were modeled with an improved version of a simplified apple tree carbon balance model (Lakso and Johnson, Acta Hort. 276:141, 1990). New and improved submodels were developed on (a) spring leaf area development and autumn leaf fall, (b) partitioning of carbon to the organs of the tree, and (3) fruit growth and abscission based on carbon balance. Simulations of known effects of low light and foliar pest damage on apple fruit growth and abscission were realistic and similar to experimental results. Similarly, long-term simulations were run of leaf area development, light interception, canopy photosynthesis and canopy respiration in different climates using temperature and radiation data from New York, New Zealand and Washington State. Simulations suggest that mid-to-late-season differences were the most distinguishing among climates, and that early season differences were less when expressed as time after budbreak. Total canopy photosynthesis over the season was estimated to be approximately 18, 23 and 25 kg fixed CO2 for a mature slender spindle tree at 2000 trees/ha using NY, WA and NZ weather, respectively. Seasonal canopy respiration was simulated to be about 13-15% of the fixed carbon for all climates. Simulations of short-term responses to low light and foliar pests and the long-term climatic simulations suggest that the model in general is behaving realistically. Keywords: fruit abscission, fruit growth, leaf area development, photosynthesis, radiation, respiration, temperature Introduction Apple orchard productivity varies greatly in different climates or different years in a one climate, but it is difficult to determine the critical factors over such a range of climatic conditions. Also, the large, perennial nature of apple trees limits classic growth analyses on cropping trees in the field, although some have been done (Forshey et al., 1983; Palmer, 1988). The lack of a great number of growth analyses in different climates reduces our ability to understand and predict climatic effects on productivity. Consequently, a sound model of short and long-term climatic effects on apple trees would be helpful to integrate empirical data, and to help explain and ultimately predict tree responses to the environment. Such results would help improve understanding, help focus research on key principles, and provide specific hypotheses to test. Over the past 25 years there have been several attempts to model apple productivity. Some models have emphasized sunlight interception by different orchard designs (reviewed in Jackson, 1980; Palmer, 1989; and Wagenmakers, 1991) and were helpful in clarifying some important interrelationships of orchard design, light interception and productivity. More complex physiologically-based models have been attempted (Cervenka, 1977; Thorpe et al., 1978; Landsberg, 1979; Elfving et al., 1983) but these were not well described or difficult to work with due to the complexity of their structure and the computer programming used. Thus, the usefulness of these models has been primarily limited to those who developed them. One important use of a realistic, easy-to-use model of carbon balance would be to compare the effects of varying climates with long-term weather data to try to understand how much of the marked differences in yields among production regions is related to environmental versus management effects on carbon balance. It is especially interesting to elucidate the reasons why New Zealand has such high yields compared to many other regions. Another goal is to understand the effects of short-term effects such as low light or effects of foliar pests on fruit development and fruit abscission. Description of the Model The current model is a modification of the original daily time-step model of leaf development, photosynthesis and respiration as described by Lakso and Johnson (1990) using Stella® dynamic modeling software. The model begins at budbreak. The major components of the model are: leaf area development/abscission, daily gross canopy photosynthesis (from Charles-Edwards, 1982), respiration of organs, carbon partitioning, and fruit development/abscission. Improvements were made to the original leaf area development submodel. New submodels were added to simulate autumn leaf abscission, partitioning of carbon among organs, and fruit growth and abscission. The parameter values in the current model are based on summarized data on many apple cultivars from the literature and our studies, but much of the data and the fruit growth components are based on our studies of 'Empire' apples. The “standard” tree simulated is a mature slender spindle 'Empire'/M9 at approximately 2000 trees/ha. This was chosen since we have done considerable research on light interception, tree and fruit development and physiology in such orchards and the chosen tree size and form is fairly common in most apple production regions. Therefore, we can better evaluate whether the simulation outputs are realistic. Required inputs. There are two types of required inputs: tree descriptions and weather data. To describe the tree, initial inputs are required of numbers of long and short shoots, numbers of flowers, spacing, and wood surface area (from surface area-to-trunk cross sectional area regressions). Default seasonal curves of photosynthesis and respiration can be accepted, or modified to reflect cultivar or seasonal differences. The required weather data is daily maximum and minimum temperatures and daily total radiation. Leaf area development and abscission submodel. Leaf area development is driven by accumulation of growing degree days, a leaf area expansion rate per degree day, total shoot numbers and the fraction of shoots that are growing at any time. The original leaf area development model used one growth function for all shoots and did not model leaf abscission in the autumn. The current version divides the shoots into long extension shoots (>5 cm) and short rosette-type shoots (spurs with bourse shoots <5 cm and short lateral shoots from 1-year-old wood). Each shoot type has a different leaf area expansion rate based on growth studies in 'Empire' and other apple cultivars. Shoot termination is artificially constrained as we have not yet developed a good understanding of regulation of shoot termination. Simulated spring leaf area development of pruned and unpruned 'Empire' trees fit published data (Lakso, 1984) reasonably well (Fig. 1). The leaf abscission in the autumn is based on multiple-year leaf drop studies done in New York and Hawkes Bay, New Zealand, representing a range of observed leaf area durations. Since both locations have similar latitudes of 41-44˚, the differences were primarily due to temperature differences. Based on these data and other observations (Jonkers,1980), the leaf abscission submodel was based on an accumulation of daily minimum temperatures below 5˚C in the autumn, similar to chill unit models. 2 Leaf area (m /tree) 10 8 6 unpruned - actual unpruned - simulated pruned - actual pruned - simulated 4 2 0 0 200 400 600 800 o Growing dregree days after budbreak (base C) 4 Figure. 1. Actual and simulated leaf area development on pruned and unpruned 'Empire' apple trees (measured data from Lakso, 1984) as a function of degree-days above 4˚C. Photosynthesis and respiration. The canopy photosynthesis equation of Charles-Edwards (1982) and leaf, structural wood and fruit respiration components have remained the same as in the original model. Current parameter values that have been improved or confirmed by recent measurements of leaf photosynthesis or organ respiration rates. Carbon Partitioning Submodel. After net CO2 exchange is calculated from canopy photosynthesis - organ respiration, the partitioning of the accumulated fixed carbon is adapted from Buwalda’s kiwifruit vine model (Buwalda, 1991). The total demand for each type of organ is estimated from its numbers and estimated maximum growth rates (typically estimated from growth studies under assumed optimum conditions for growth). Shoot and fruit demands were estimated from growth studies, but root and wood demands were mostly guesses. The total demand for an organ is equal to the maximum growth demand (adjusted for temperature) times the number of active organs of that type. If adequate carbon is available to fully support all organs , the carbon is partitioned equal to the demands and maximum growth occurs for all organs. However, if the carbon supply is less than the total demand, a prioritization was used. A “relative sink strength” (RSS) factor was estimated for each type of organ, and the total of the RSS factors equal 1.0. Based on review of the literature and our own studies, the relative sink strengths were chosen to be in the following order: shoots>>fruits>roots=wood. This gave strong priority to shoots so that early in the season when shoots are active, they receive a greater proportion of their demand. Later, as shoots terminate growth, the partitioning shifts to fruits and other organs even though the RSS values remain constant. This is consistent with studies that indicated that shoot tips were very strong competitors for carbon in the early season and that under low light conditions, carbon partitioning to fruit or fruit growth suffered much more than did shoot growth (Quinlan and Preston, 1971; Corelli Grappadelli et al., 1994; Bepete and Lakso, 1998). The actual amount partitioned to each organ type depends on the individual demands, the number of actively-growing organs (e.g. number of active shoots), and whether carbon is adequate or limiting. The relative partitioning to a given organ (RPi) is estimated by: RPi = DemandI - (DemandI (1-RSSi)(1 - (Carbon avail / Demand total) The actual carbon partitioned then to each organ is: Carboni = RPi (Carbon avail / ∑ RPi ) Fruit abscission and growth submodel. To simulate the effects of carbon supply on the growth and abscission of the fruit, fruit abscission occurs if fruit growth rate is not maintained above a critical rate. This relationship was based on several studies of growth rates and abscission of different cultivars in response to different treatments such as Naphthaleneacetic acid (NAA) thinning sprays or heavy shading. Although there was variation, a consistent pattern of fruit abscission occurred if fruit growth rates were not maintained above about 60% of the rate of the fastest-growing fruits in the population (Fig. 2). We found that the relationship was more consistent if the growth rates were expressed relative to the fastest-growing fruits in each study rather than to any specific absolute growth rates. Whether further improvements will occur if relative growth rates (RGR) are used is being explored. Fruit abscission (%) 100 Delicious '91 Gala '91 Empire '91 - 20mm Empire '93 - 7mm Empire '93 - 18mm Empire '86 - 10mm Empire '86 - 24mm 80 60 40 20 0 0 20 40 60 80 100 Fruit growth rate as % of fruit with highest growth rate Figure 2. The relationship between fruit abscission and fruit growth rate as % the fastest growing fruits in a population in several NAA or shade studies (unpublished data of A. Lakso). The fruit growth/abscission model operates by comparing the amount of fruit growth supported by the carbon partitioned to fruit each day with a 3-day running average (to simulate the observed buffering of single day variations) to the maximum growth expected on that day (based on a maximum growth rate curve and the number of fruits on the tree at that time). The % of maximum growth supported is used to cause fruit abscission as described above. As fruit abscise, the number of current fruit decreases for the next daily cycle. The fruit growth that is supported is accumulated to give the total crop weight and mean fruit weight. Simulations of Short and Long-Term Climatic Variation Climate Comparisons. Long-term mean daily weather data and average budbreak dates were obtained for Geneva, NY (20 year mean, latitude 43˚ N), Prosser, Washington (4 year mean, latitude 46˚N courtesy of R. Wample) and Havelock North, New Zealand (4 year mean, 40˚ S latitude). The climate data was used to drive the model. It was decided to use the "standard tree" to emphasize climate differences and to avoid the confounding effects of different training systems or tree sizes, etc. The trees were constrained to stop at the same final leaf area (about 14 m2/tree) and same final light interception (about 52% at full canopy). It is recognized that apple trees may grow for longer periods in different climates, but that aspect will be modeled later. The climatic differences can be summarized as follows: • New York (NY) had the shortest growing season, shortest leaf area duration (LAD) and the lowest amount of total radiation available and intercepted. Temperatures were intermediate among the 3 climates and showed less diurnal amplitude than in New Zealand and Washington. • New Zealand (NZ) allowed the longest LAD, the least extreme climate due to the marine influence, and the coolest summer and warmest winter temperatures. • Washington State (Wa) is a slightly longer season than NY, but shorter than NZ. There are more clear days so there is higher radiation mid-season, with the warmest maximum temperatures and cool minimums. Since climate comparisons are begun at apple budbreak, the three climates are surprisingly similar in the first 30-50 days since the tree development requires similar temperatures to begin regardless of the rest of the growing season. The greatest differences are in the length of the seasons and the amount of postharvest activity. This is reflected in the simulated seasonal patterns of canopy photosynthesis and respiration (Fig. 3). They suggest that early-season differences are relatively small, but that mid and lateseason differences are quite large, reflecting the differences in LAD. Wünsche et al. (2000) with whole canopy chambers reported similar results, except that they found much higher NCE rates at 211 days after bloom than our model. The seasonal cumulative light-period canopy photosynthesis (does not include lightperiod respiration by fruits, wood, etc.) was simulated to be about 18, 23 and 25 kg of fixed CO2 per tree in NY, Wa and NZ respectively, a range of almost 40%. Seasonal cumulative total respiration loss (24-hour fruit and wood plus dark leaf respiration) was estimated at 13-15 percent of the fixed CO2 in all climates. This gave net cumulative CO2 fixation per tree per year of about 16, 19 and 22 kg/tree in NY, Wa and NZ respectively. The respiratory losses are very low compared to most plants (Amthor, 1989), but they are reasonable compared to our previous studies with direct measurement by “balloon” chambers. We found night respiration rates of 5-20% of daily fixed CO2 following sunny days at different times of the season (Lakso and Piccioni, unpublished data). Studies in NZ by Wünsche et al. (2000) found that night respiration in the cool nights of NZ to give even smaller percentage respiratory losses. 2 /day) Daily canopy photosynthesis (g CO 180 150 120 90 NZ 60 NY Wa 30 0 0 30 60 90 120 150 180 210 240 270 300 Days after budbreak Figure 3. Simulated daily canopy photosynthesis of modeled 'Empire'/M.9 slender spindle trees at 2000 trees/ha using long-term weather data from Geneva, NY, Prosser, WA and Havelock North, NZ. Simulations of short-term light effects. During the early period after bloom when final fruit numbers are set and cell division occurs in the fruit, fruit abscission is known to be quite sensitive to low light or high temperatures. Byers et al. (1991) showed that at 30 days after bloom fruit abscission could be increased by very low light if it occurred more that 2 consecutive days, but that single days of low light had no effect. This general effect was simulated by reducing the radiation input at a similar time of the season to 4 MJ/m2 (about 15% of that on a clear sunny day that reduced simulated canopy photosynthesis by 73%) for 1, 2 or 3 days continuously or 2 and 3 days of low light alternated with days of full sunlight. The simulations were realistic to the low light treatments at that time with 1 day of low light causing no fruit abscission, 2 days causing some abscission, and 3 days causing heavy abscission (Fig. 4). If alternated with sunny days, 2 or 3 days of low light caused partial abscission. Byers, et al. (1991) found similar experimental responses although our simulations indicated a stronger effect of 3 continuous days of low light. Simulations of foliar pest effects. A second simulation test of the fruit development model was to simulate the effects on fruit growth of a severe mid-season European Red Mite infestation (cumulated mite-days of about 2000) as measured experimentally by Francesconi et al. (1996). The model used long-term average NY weather and simulated the mite effect by reducing the light-saturated leaf photosynthesis rate (Pmax) at 110 days after budbreak by 40% as found in the actual study. The seasonal fruit growth curves of our "standard" fully-cropped trees with and without the simulated leaf damage were found to be quite similar to those found experimentally (Fig. 5). This suggests that the model is realistic in modeling mid-to-late season fruit growth effects. Fruit number as % of untreated 100 Byers et al., 1991 Simulated 80 60 40 20 0 None 1 Day 2 Day 3 Day 2/Alt 3/Alt Low light treatments Figure 4. Effects of 1, 2 or 3 days of continuous low light or 2 or 3 days of low light alternated with sunny days on actual (Byers, et al., 1991) and simulated relative fruit drop. Mean fruit weight (g) 200 Actual - control Simulated - control Actual - 2000 cmd Simulated - 2000 cmd 160 120 80 40 0 0 30 60 90 120 150 Days after bloom Figure 5. Patterns of fruit growth as affected by a severe mid-season European Red Mite infestation (2000 cumulative mite-days) as determined experimentally by Francesconi et al. (1996) and simulated by reducing the leaf Pmax at 80 days after bloom by 40% as found in the actual study. Summary We have developed an extended version of the simplified apple carbon balance model. 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