Knowledge about the seasonal dynamics of tree growth and its relationship with environmental factors is necessary to eliminate the uncertainty due to ongoing climate change and for more precise growth modelling when re-measurements are done periodically. Despite the increasing number of studies monitoring seasonal wood formation, a considerable part of European forests, including Estonia, lacks such information. In this article, we present a date-dependent model for determining the share of seasonal radial growth for the three most common tree species in the region (Scots pine, Norway spruce and silver birch) for Estonian conditions. Since seasonal tree growth monitoring data were unavailable for Estonia, we used published seasonal radial growth data from Lithuania by Dr Adomas Vitas (2011). We tested four functions (Kumaraswamy, Weibull, Gompertz and logistic) on obtained data to approximate the seasonal development of radial growth. Kumaraswamy's function could track the course of seasonal radial growth gains the best; thus, this function was chosen for further use. We obtained data on intra-annual radial growth from published research studies from neighbouring countries and determined the dates of growth initiation and cessation for Estonian conditions. Finally, we combined Kumaraswamy's function and the predicted radial growth onset and cessation dates into the model that could predict the seasonal growth course and thus were able to estimate the share of newly formed increment from the dates. Knowledge of the seasonal dynamics of tree growth and its relationship with environmental factors is necessary to eliminate climate change's current uncertainty and to model growth accurately. Despite the increasing number of studies on the seasonal growth of trees, such knowledge is lacking in a significant part of Europe, including the Estonian hemiboreal forest. To accurately determine the time between two measurement occasions in the Estonian Network of Forest Research Plots data analysis, it is necessary to consider how much intra-annual growth has been formed at the moment of the re-measurement occasion, because measurement dates usually do not coincide. In this article, we present a model that enables predicting tree seasonal cumulative relative growth at any date for environmental conditions in Estonia. Since seasonal tree growth observations in Estonia are still ongoing, the relative radial growth model developed in this study relies on data of neighbouring countries. We used growth data for Scots pine, Norway spruce and silver birch published by Vitas (2011) which describes relative radial growth over the season. We tested four sigmoid functions (Kumaraswamy (equation 1), Weibull (equation 2), Gompertz (equation 3) and logistic (equation 4)) to model the intra-annual growth dynamics. Guided by the nature of the seasonal growth process of trees, we chose the Kumaraswamy function to estimate the cumulative relative radial growth of trees. For silver birch, this function also had the smallest residual standard error on Vitas' (2011) data, however, for conifers, a statistically better fit was obtained with the Weibull function (Table 2 , Figure 1). For the selected function to correctly determine the course of growth, the beginning (onset) and end of growth are necessary to ascertain, but currently these data are still not available for Estonia. Thus, we used the published research data from neighbouring countries, Lithuania and Finland (Table 1). Since Estonia is located north of Lithuania, the growing season in Estonia probably starts later and ends earlier. There are several studies about Finland where the seasonal growth of trees should start later and end earlier than in Estonia (Jyske et al. , 2014 ; Mäkinen et al., 2008 ; Schmitt et al. , 2004). The data of the beginning (A) and end (B) of the seasonal radial growth of trees collected from the scientific literature (Table 1) were approximated with a linear model (equation 5). The linear model (equation 5) results (Table 3 , Figure 2) revealed that the beginning and end of the seasonal radial growth of the trees depend on the geographical latitude (LAT) and the measurement method (M). The effect of the tree species (PL) factor was not statistically significant in this model. By predicting the onset A and end B of the seasonal radial growth with equation 5 for Estonian conditions (geographic north latitude 58.5 degrees and dendrometer method), we obtained 132.2 and 238.5, respectively, for Scots pine, 132.2 and 234.1 for Norway spruce and 134.6 and 233.7 days for silver birch from the beginning of the year. Using the above estimates, Figure 3 presents the model predictions of the seasonal relative radial growth with the Kumaraswamy function (equation 1 , Table 2) for Estonian conditions. The beginning and end of the growth period varies from year to year (Tarand et al., 2013). Our model is universal, so the user can determine the start and end day of growth according to the weather conditions and geographical location (Western Estonian islands vs South-Eastern Estonia). Further research is needed for this. In order to obtain a more accurate model of intraseasonal growth dynamics and for other tree species in Estonia, it is necessary to carry out long-term, labour-intensive research. [ABSTRACT FROM AUTHOR]