The Influence of Urban Conditions on the Phenology of Aesculus hippocastanum L. Using the Example of Wroclaw (Poland)

Abstract

The differences in plant phenology between rural and urban areas are the subject of research conducted all over the world. There are few studies aimed at assessing the impact of the urban heat island on plant vegetation only in urban areas. The aim of this study is to assess the impact of the distance from the city center and the form of land cover on the phenological development of trees using the example of the horse chestnut (Aesculus hippocastanum L.). The research area covered the entire city of Wrocław. In order to best capture the impact of the distance from the city center on the rate of changes of individual phenophases, 3 areas were designated—at a distance of 1 km, 2 km and 5 km. The study assessed the average duration of individual phenological phases along with the variability characteristics for leafing, flowering and fruiting in relation to the designated zones and classified forms of land cover based on mean value ($\overline{x}$) and standard deviation (±SD) in individual weeks of the year. For the leafing and flowering phases, the frequency of the occurrence of phases in individual weeks of the year was analyzed in relation to the designated zones and classified land use methods. The results obtained on the basis of phenological observations carried out in 2017 in Wrocław confirmed the extension of the period of vegetation in the city center in relation to its peripheries. Trees growing in road lanes entered the vegetation period later and defoliated faster, which confirms the negative impact of street conditions on the development of trees in urban space. Thus, the growing season in road lanes is shorter and due to the 1-year observation period, it is justified to conduct further observations.

1. Introduction

There are numerous studies around the world showing the impact of urbanization and global climate change on the environment [1,2,3,4,5,6,7,8,9,10,11]. Urban conditions can significantly influence plant phenology by modifying the hydrological regime or the local climate [12]. Škvareninová et al. [13] or Ffrench-Constanti et al. [14] also proved the influence of artificial lighting on the phenology of urban plants. Ballester et al. [15], Seto et al. [16] and Klemm et al. [17] showed that urbanized regions can be much warmer than the surrounding rural regions, creating a so-called urban heat island (UHI). McCarthy et al. [18] or Oleson et al. [19] emphasize the topicality and importance of research on UHI and related aspects, especially because the percentage of the world’s population inhabiting urban areas is increasing and high temperatures can affect the thermal comfort and well-being of the urban inhabitants [20]. Cities are an important area of phenological research because their warmer conditions can help to assess the potential effects of climate change on plants [4,21,22]. Temperature trend analyses over 100 years in some cities in the United States showed that the temperature in urban areas from 1940 to 2000, increased by an average of 0.5–3.0 °C [23]. Cardelino and Chameides [24] showed that in Atlanta, in the 15 years to 1990, there was an increase in air temperature of about 2 °C during the summer period due to the progressive urbanization and the accompanying intensification of the urban heat island. Increasing thermal contrast between the city center and the city peripheries was also noted in European countries, including in Athens [25] or in London [26].

However, little is known about the spatial and temporal variability of plants as a result of the interaction between urban conditions and UHI [27]. The increase in temperature caused by the urban heat island affects the phenology of plants both within and around cities [28,29,30,31], unfortunately, the ecological impact of urban heat island remains poorly understood in scientific research [27,31,32].

The differences in plant phenology between rural and urban areas are the subject of research conducted all over the world, both in Europe [10,21,29,30,33,34] and in North America [12,33,34,35,36], South America [30], Asia [33,37,38,39] or Africa [33]. However, these studies, which are mainly based on the observations of one or several species, do not aim to capture the variability within cities [21,40]. There are few studies aimed at assessing the impact of the urban heat island on plant vegetation only in urban areas [23,27,34,41].

Due to the difficulty and time consuming nature of conducting phenological observations, many researchers rely on satellite remote sensing to investigate spatial variability [27,35,42], limiting themselves only to capturing the beginning and end of the growing season. Moreover, these studies omit the assessment of the influence of city geometry, land use or tree growth conditions on their phenology, which is an important gap in phenological research, as emphasized by Jochner et al. [29] and Walker et al. [43], basing their observations on only one type of space, for example, forest areas, as did Fisher et al. [44] or Elmore et al. [42]. On the other hand, Zipper et al. [27] took into account two types of areas—wooded and sodded areas. Taking into account the spatial aspect is of particular importance in the context of the results of Yang et al. [45] or Masiero and Souza [46], showing the influence of the type of urban area on thermal conditions.

The aim of this study is to assess the impact of the distance from the city center and the form of land cover (surrounding area) on the phenological development of trees using the example of the horse chestnut (Aesculus hippocastanum L.).

2. Materials and Methods

2.1. The Range of Research

Wrocław is located in south-western Poland, in the center of the Silesian Lowland (51_ N, 17_ E) on the Odra River and its four tributaries (Figure 1). It is the historical capital of Silesia and Lower Silesia. The altitude above sea level ranges from 105 to 145 m. The city has approximately 640,000 inhabitants and its area is 293 km², including 31.4% built-up areas, 36.6% green areas and 28.9% agricultural areas and water (3.1%).

Wrocław is located in the temperate climate zone of the northern latitude, in a transitional type of climate, subject to oceanic and continental influences. The average annual air temperature in Wrocław is 9.0 °C, with lows in the coldest month (January) of around −0.4 °C and highs in the hottest month (July) of around 18.8 °C. The amplitude of the annual temperature, which is a measure of the degree of climate continentalism, is 19.2 °C. Atmospheric precipitation occur on 167 days a year and the average annual rainfall in the years 1901–2000 is 583 mm [47]. The vegetation period in Wrocław in the years 1951–2014 was 237.6 days on average and the sum of active temperatures was 174.4 days, which qualifies Wrocław as one of the cities with the longest vegetation period in the south-western Poland [48].

In the year 2017, from March to September, the mean monthly air temperature values for each month were higher than the mean air temperature value for the years 1951–2017 (Figure 2a). In the summer months, from June to July, these values were even 7 °C higher. On the other hand, November, December and January were characterized by lower average air temperature values compared to the multiannual period average.

In April and July 2017, monthly rainfall totals were much higher than the average values of the compared multiannual period (Figure 2b). Moreover, higher precipitation has been documented in September and October. On the other hand, lower rainfall totals were recorded in May; they were more than three times lower in comparison (approx. 18 mm) than the average value of the 1951–2017 period (60 mm). In the summer months, except for July, lower rainfall was recorded compared to the multiannual period average. Whereas, in March and February the rainfall was close to the mean values in terms of quantity.

The research area covered the entire city of Wrocław. In order to best capture the impact of the distance from the city center on the rate of changes of individual phenophases, 3 rays were designated (the pillory in the city center in Wrocław, 51°06′34.1′′ N 17°01′57.7′′ E, was taken as a reference point)—at a distance of 1 km (R1), 2 km (R2) and 5 km (R3). The rays were determined with regard to the structure and type of buildings, green areas and UHI temperature distribution developed for Wrocław by Szymanowski and Kryza [50]. These rays were determined in such a way that the first area covered the strict city center (zone 1—Z1), the second area was with dense historic quarter buildings (zone 2—Z2) and a third area with looser buildings and larger green areas (zone 3—Z3), which separated the zone with the lowest degree of development, with predominantly green areas (zone 4—Z4).

2.2. Research Objects

The horse chestnut (Aesculus hippocastanum L.), brought to Europe in the 16th century, is one of the most popular species used in urban areas [51]. It has been the subject of observation in many phenology-based studies [6,52,53,54,55,56,57,58,59,60]. The horse chestnut was chosen for our research as it is a species that occurs frequently in Wrocław, its morphology allows for a precise definition of phenological phases and it is of great environmental and aesthetic importance for the city and additionally, it is characterized by early phenology.

A total of 92 objects were selected for observation (Figure 1)—including 24 located in the central area—zone 1 (Z1), 21 objects between 1 and 2 km from the center (Z2), 24 facilities in the area from 2–5 km (Z3) and 22 objects located more than 5 km from the designated center (Z4). Moreover, when selecting the objects, the form of land cover on which the tested object is located was taken into account, distinguished as follows: green areas, high-rise areas (multi-family buildings with at least 4 storeys were assumed to be high-rise buildings) and areas near communication routes and water courses and reservoirs (

Table 1. Number of objects selected for observation depending on the distance from the reference point and type of land cover (Based on [61]).

Land Cover	Urban Atlas 2006 for Wrocław	Abbrev	(Zones)				Number of Objects
			Distance from the City Centre (km)
			Z1	Z2	Z3	Z4
			0–1	1–2	2–5	>5
Green Spaces	Green urban areas	GS	8	6	6	7	27
Street Areas	Other roads and associated land	S	6	6	8	7	27
High-rise Building Areas	Continuous Urban fabric (S.L. > 80%) Discontinuous Dense Urban Fabric (S.L.: 50–80%)	HB	7	6	5	5	24
Water Areas	Water	W	3	3	5	3	14
	Total:		24	21	24	22	92

)—in determining the forms of land cover, the Urban Atlas was used [61]. All specimens were also selected taking into account their age—the units selected for the study had circumferences larger than 150 cm measured at a height of 130 cm above the ground and were of good phytosanitary condition.

2.3. Field Observations

Field observations were carried out weekly from 1 March 2017 to the end of November, 2017. In order for the assessment process to be objective, the assessment was made by one person on the basis of photographic documentation collected in the field, which included a photograph of the silhouette of the entire tree and details such as buds, leaves, inflorescences, fruits. We have attached an observation sheet as Supplementary Material (Table S1).

The phenological observations were based on BBCH (Biologische Bundesantalt, Bundessortenamt and Chemische Industrie) code after Finn et al. [62]. The BBCH scale has been applied so far in phenological observations of non-cultivated woody plant species Babálová et al. [63] in the studies on small-leaved linden, hawthorn, common hazel, blackthorn, by Lukasová et al. [64] examining the common beech or by Stratópoulos at al. [65]. A uniform method of presentation and determination of individual phenological phases was adopted, as specified in

Table 2. Division and description of phenophases (based on BBCH code).

No. of Phenological Phase	BBCH Code	Phenological Phase	BBCH Code Description
Ph0	BBCH 00	Leaf buds closed	Buds closed and covered by scales
Ph1	BBCH 07	The beginning of the opening of leaf buds	Beginning of sprouting or bud breaking
Ph2	BBCH 11	The beginning of spreading the leaf blades	First leaves unfolded
Ph3	BBCH 19	Full foliation	Leaf expansion complete
Ph4	BBCH 93	The beginning of leaf fall	Beginning of leaf fall
Ph5	BBCH 97	The end of leaf fall	End of leaf fall
Ph6	BBCH 511 *	The appearance of the inflorescence	Undeveloped inflorescences are noticeable
Ph7	BBCH 512 *	The full appearance of the inflorescence	Fully developed inflorescences are noticeable
Ph8	BBCH 62	The beginning of flowering	20% flowers open
Ph9	BBCH 652 *	Full flowering	above 70% of flowers open
Ph10	BBCH 671 *	The flowering finishing	50% of petalas fallen or dry
Ph11	BBCH 69	The end of flowering	Fruit are visible
Ph12	BBCH 79	Full ripening of fruit	80% of fruits have reached final size
Ph14/13	BBCH 89	The end of fruit ripening	fruits fully ripe

* code extension for the purpose of the article.

. For the purpose of our research, like in Delgado at al. [66] or Cosmulescu and Scrieciu [67], the BBCH scale has been modified—it has been extended to four new phases marked with an asterisk in Table 2.

2.4. Data Analysis

The study assessed the average duration of individual phenological phases along with the variability characteristics for leafing, flowering and fruiting in relation to the designated zones and classified forms of land cover based on mean value ($\overline{x}$) and standard deviation (±SD) in individual weeks of the year and Julian days.

Moreover, length estimates were performed for the vegetative phases of phenological development duration of individual phases in relation to each other. This length was determined based on the differences between the averaged dates of the observed phases of vegetative development.

In order to verify the statistical significance in relation to comparable groups of trees growing in the designated zones, the t- Student test was performed at the level of p < 0.05.

For the leafing and flowering phases (Ph1–Ph11), the frequency of the occurrence of phases in individual weeks of the year was analyzed in relation to the designated zones and classified land use methods.

3. Results

3.1. Influence of Distance from the Centre on Phenological Development

The results obtained on the basis of the average time of occurrence of phenological phases for the adopted zones showed that in 2017, the beginning of vegetation was observed faster in the city center than on its periphery (

Table 3. Average onset ($\overline{x}$) date and standard deviation (SD) of occurrence of individual phenological phases depending on the distance from the city center [in weeks and Julian days].

No. of Phenological Phase	BBCH Code	Zone
			Z1	Z2	Z3	Z4
Leaves ($\overline{\mathit{x}}$ ± SD)
Ph1	BBCH 07	J. days	86 ± 3	87 ± 5	89 ± 5	91 ± 7
		week	12.5 ± 0.5	12.5 ± 0.7	13.0 ± 0.7	13.5 ± 0.9
Ph2	BBCH 11	j. days	94 ± 5	95 ± 5	99 ± 6	100 ± 4
		week	13.6 ± 0.6	13.9 ± 0.5	14.1 ± 0.7	14.2 ± 0.5
Ph3	BBCH 19	J. days	119 ± 5	119 ± 7	122 ± 9	124 ± 6
		week	16.8 ± 0.7	16.6 ± 0.9	17.5 ± 1.3	17.6 ± 0.9
Ph4	BBCH 93	J. days	264 ± 24	261 ± 20	263 ± 28	262 ± 17
		week	38.0 ± 3.4	37.7 ± 2.8	37.8 ± 3.8	38.0 ± 2.3
Ph5	BBCH 97	J. days	317 ± 9.8	311 ± 13	312 ± 12	311 ± 8
		week	45.5 ± 1.4	44.6 ± 1.8	44.7 ± 1.8	44.6 ± 1.1
Flowers and Fruits ($\overline{\mathit{x}}$ ± SD)
Ph6	BBCH 511	j. days	99 ± 5	99 ± 6	102 ± 6	104 ± 5
		week	14.2 ± 0.7	14.1 ± 0.8	14.6 ± 0.9	14.0 ± 0.7
Ph7	BBCH 512	J. days	109 ± 6	111 ± 7	113 ± 6	116 ± 5
		week	15.7 ± 0.8	15.8 ± 0.9	16.2 ± 0.8	16.0 ± 0.7
Ph8	BBCH 62	J. days	119 ± 6	120 ± 7	124 ± 7	126 ± 4
		week	16.9 ± 0.8	17.1 ± 1.0	17.5 ± 1.0	18.0±0.7
Ph9	BBCH 652	J. days	131 ± 4	133 ± 5	137 ± 5	138 ± 4
		week	18.7 ± 0.6	18.9 ± 0.8	19.5 ± 0.7	19.0 ± 0.5
Ph10	BBCH 671	J. days	143 ± 4	144 ± 5	146 ± 5	145 ± 5
		week	20.4 ± 0.9	20.7 ± 0.8	20.9 ± 0.7	20.0 ± 0.7
Ph 11	BBCH 69	J. days	157 ± 6	158 ± 10	157 ± 7	157 ± 7
		week	22.3 ± 0.7	22.5±1.3	22.4 ± 0.9	22.0 ± 0.9
Ph 12	BBCH 79	J. days	193 ± 9	200±13	206 ± 17	205 ± 16
		week	27.8 ± 1.3	28.7±1.8	29.7 ± 2.5	29.6 ± 2.5
Ph 13	BBCH 89	J. days	240 ± 22	241±18	244 ± 15	245 ± 9
		week	35.0 ± 3.1	34.6±2.6	35.1 ± 2.4	35.4 ± 1.5

). The growing season in the city center also lasted longer, on average from mid-12 weeks (i.e., 4th week of March) to the middle of the 45th week of the year (i.e., 2nd week of November), while on the periphery of the city, from the middle of the 13th week (i.e., 1st week of April) to the middle of the 44th week of the year (i.e., 1st week of November).

The phenological phases “The beginning of the opening of leaf buds “(BBCH 07) and “The beginning of spreading the leaf blades” (BBCH 11) were first observed in trees growing in zone Z1 (Table 3). Compared with trees growing in other areas, this difference was approximately one week, occurring in the final third of March. The “Full foliation” (BBCH 19) of trees growing in zones Z1 and Z2 occurred about 1 week earlier than in trees growing in zones Z3 and Z4. The Ph3 phase for trees growing at a distance of 2–5 km showed the greatest variability, over 1 week, while trees growing in the center showed almost two times less variability. The “The beginning of leaf fall” (BBCH 93) was characterized by the greatest variability among all vegetative phases, from 2 to even 4 weeks in individual zones. The lowest variability was recorded in the area located more than 5 km from the center, that is, in zone Z4. The highest variability was documented in zones Z1 and Z3. The average time of “end of leaf fall” (Ph5) occurred at a similar time in all zones. The most noticeable differences were observed between trees growing in zones Z1 and Z2, in which the variability of this phase was smaller compared to trees growing in zones Z3 and Z4.

“The appearance of the inflorescence” (BBCH 511*) was observed the earliest in zones Z1 and Z2, at the beginning of the 14th week of the year (Table 3). The “The beginning of flowering “(BBCH 62) occurred on average in the 17th week of the year for trees growing in the city center in zones Z1 and Z2 and a week later for trees growing in zone Z4. The “Full flowering” (BBCH 671*) were first recorded on trees within 1 km (zone Z1), while in the remaining zones, the appearance of this phase was similar in time. “The end of flowering “(BBCH 69) was recorded simultaneously on all trees, regardless of the distance from the center of Wrocław.

The appearance of the phenological phases concerning fruiting in all trees was similar, regardless of the designated zone (Table 3). These phases were characterized by the greatest variability among all phenological phases, especially “Full ripening of fruit” (BBCH 79) and “The end of fruit ripening” (BBCH 89).

Table 4. Duration of the vegetative phases (Ph1-Ph5) in 2017, for trees in individual zones (Z) (in weeks).

Z1		Ph1	Ph2	Ph3	Ph4	Ph5	Z3		Ph1	Ph2	Ph3	Ph4	Ph5
	Ph1		-	-	-	-		Ph1		-	-	-	-
	Ph2	1.1		-	-	-		Ph2	1.1		-	-	-
	Ph3	4.3	3.2		-	-		Ph3	4.5	3.4		-	-
	Ph4	25.5	24.4	21.2		-		Ph4	24.8	23.7	20.3		-
	Ph5	33.0	31.9	28.7	7.5			Ph5	31.7	30.6	27.2	6.9
Z2		Ph1	Ph2	Ph3	Ph4	Ph5	Z4		Ph1	Ph2	Ph3	Ph4	Ph5
	Ph1		-	-	-	-		Ph1		-	-	-	-
	Ph2	1.4		-	-	-		Ph2	0.7		-	-	-
	Ph3	4.1	2.7		-	-		Ph3	4.1	3.4		-	-
	Ph4	25.2	23.8	21.1		-		Ph4	24.5	23.8	20.4		-
	Ph5	32.1	30.7	28.0	8.9			Ph5	31.1	30.4	27.0	6.6

Ph1–BBCH 07; Ph2–BBCH 11; Ph3–BBCH 19; Ph4–BBCH; Ph5–BBCH.

shows the duration of the individual vegetative phases on the basis of the difference between the averaged dates of phase appearance. The greatest differences in the length of the growing season of horse chestnut, from the cracking of leaf buds to the end of leaf fall, were documented between trees growing in zone Z1 and trees in zone Z4—a difference of almost 2 weeks. However, the difference between trees growing in zones Z1 and Z2 is about 1 week, between zones Z2 and Z3, only half a week and for Z2 and Z4, it is again 1 week.

On the basis of the t-Student test (

Table 5. The values of Student’s t-test for phenological phases (Ph) of leaves and flowers between trees, growing in individual zones (Z1–Z4) of the city.

Leaves
Ph0 (BBCH 00)		Ph1 (BBCH 07)		Ph2 (BBCH 11)		Ph3 (BBCH 19)		Ph4 (BBCH 93)		Ph5 (BBCH 97)
Zone	t	Zone	t	Zone	t	Zone	t	Zone	t	Zone	t
Z1:Z2	-	Z1:Z2	-	Z1:Z2	-	Z1:Z2	-	Z1:Z2	-	Z1:Z2	-
Z2:Z3	-	Z2:Z3	−2.07 **	Z2:Z3	-	Z2:Z3	-	Z2:Z3	-	Z2:Z3	-
Z3:Z4	-	Z3:Z4	-	Z3:Z4	-	Z3:Z4	-	Z3:Z4	-	Z3:Z4	-
Z1:Z3	-	Z1:Z3	−2.6 *	Z1:Z3	−2.55 *	Z1:Z3	−2.03 **	Z1:Z3	-	Z1:Z3	2.04 **
Z1:Z4	-	Z1:Z4	−3.28 *	Z1:Z4	−3.72 *	Z1:Z4	−3.26 *	Z1:Z4	-	Z1:Z4	2.6 ***
Z2:Z4	-	Z2:Z4	−2.78 *	Z2:Z4	−2.13 **	Z2:Z4	−2.35 **	Z2:Z4	-	Z2:Z4	-
Flowers
Ph6 (BBCH 511)		Ph7 (BBCH 512)		Ph8 (BBCH 62)		Ph9 (BBCH 652)		Ph10 (BBCH 671)		Ph11 (BCCH 69)
Zone	t	Zone	t	Zone	t	Zone	t	Zone	t	Zone	t
Z1:Z2	-	Z1:Z2	-	Z1:Z2	-	Z1:Z2	-	Z1:Z2	-	Z1:Z2	-
Z2:Z3	-	Z2:Z3	-	Z2:Z3	-	Z2:Z3	−2.87 *	Z2:Z3	-	Z2:Z3	-
Z3:Z4	-	Z3:Z4	-	Z3:Z4	-	Z3:Z4	-	Z3:Z4	-	Z3:Z4	-
Z1:Z3	-	Z1:Z3	−2.21 **	Z1:Z3	−2.62 *	Z1:Z3	−4.26 *	Z1:Z3	-	Z1:Z3	-
Z1:Z4	−3.24 *	Z1:Z4	−3.73 *	Z1:Z4	−5.14 *	Z1:Z4	−6.17 *	Z1:Z4	-	Z1:Z4	-
Z2:Z4	−3.14 *	Z2:Z4	−2.76 ***	Z2:Z4	−3.36 *	Z2:Z4	−4.33 *	Z2:Z4	-	Z2:Z4	-

t.–t-student, p = 0,01 *; p < 0,05 **; p < 0,1 ***.

), it was shown that the differences in the course of phenological phases between groups of trees distant from each other between zones Z1 and Z3, Z1 and Z4 as well as Z2 and Z4 were statistically significant. However, there were no statistically significant differences between the groups of trees growing in neighboring zones such as Z1 and Z2, Z2 and Z3 and Z3 and Z4. The analysis of the fruiting phases showed no statistical significance in relation to comparable groups. The Ph5 phase (BBCH 97—The end of leaf fall) was statistically significant only between trees growing in zones Z1 and Z3 and Z1 and Z4. There were no statistically significant differences for the leaf fall phases.

On the basis of the frequency analysis, it was shown that with increasing distance from the city center, the frequency of particular phases decreases and their duration increases at the same time (Figure 3). This regularity was especially noticeable for the initial phases Ph1 (BBCH 07) and Ph2 (BBCH 11). In trees growing in zones Z3 and Z4, a delay in individual phenological phases was observed more often. The Ph4 phase (BBCH 93) was characterized by high variability, especially up to 2 km from the city center, where in approx. 20% of horse chestnut trees, the leaves remained on the tree longer. In the case of the Ph5 phase (BBCH 97), trees growing in zone Z1 maintained their leaves longer than trees in other zones. The total defoliation of trees in the Z1 zone is initially more dynamic (individual observations in the following weeks) compared to trees growing more than 1 km from the city center. In trees growing in the Z4 zone, the Ph4 phase (BBCH 93) was recorded in more than 20% over 34 weeks, while in the center, this phase was observed only in 8% of trees. In 43 weeks, within a radius of 1 km from the center, only about 8% of trees without leaves were recorded, while in further zones it was over 40% in Z2 and over 30% in Z3 and Z4.

The assessment of the frequency of the generative development phases from Ph6 to Ph9 (BBCH: 511*, 512*, 62, 652*) showed that they took place first in the city center and with the increasing of the distance from the city center, were observed later. The full flowering of the horse chestnut tree began in the 18th week of the year. At that time, 39% and 33% of the observed specimens flourished in Z1 and Z2, respectively, while only 8.3% and 4.5% flourished in zones Z3 and Z4. In the case of phases Ph10 (BBCH 671*) and Ph11 (BBCH 69), this regularity was not so clear. On the other hand, it was noticeable that within the Z3 and Z4 zones, trees whose phenological phases were delayed in relation to trees growing in the central parts of the city were noted more often.

3.2. The Impact of Land Use on the Pace of Phenological Development

Table 6. Average date (x) and standard deviation (SD) of the occurrence of individual phenological phases depending on the form of land cover [in Julian days and weeks].

No. of Phenological Phase	BBCH Code	Zone
			Green Spaces	Street Areas	High-Rise Building Areas	Water Areas
Leaves ($\overline{\mathit{x}}$ ± SD)
Ph1	BBCH 07	j. days	86 ± 5	89 ± 6	87 ± 5	89 ± 7
		week	12.7 ± 0.7	13.0 ± 0.8	12.6 ± 0.7	12.8 ± 0.9
Ph2	BBCH 11	J. days	97 ± 5	97 ± 5	97 ± 5	100 ± 4
		week	13.9 ± 0.7	14.0 ± 0.6	13.8 ± 0.6	14.1 ± 0.5
Ph3	BBCH 19	J. days	121 ± 8	121 ± 6	119 ± 8	122 ± 6
		week	17.3 ± 1.1	17.3 ± 1.0	16.9 ± 1.4	17.4 ± 0.9
Ph4	BBCH 93	J. days	271 ± 17	251 ± 25	265 ± 22	265 ± 19
		week	38.9 ± 2.3	36.1 ± 3.6	38.0 ± 3.1	38.0 ± 2.6
Ph5	BBCH 97	J. days	314 ± 11	309 ± 9	317 ± 10	312 ± 11
		week	44.9 ± 1.6	44.3 ± 1.2	45.4 ± 1.5	44.9 ± 1.6
Flowers and fruits ($\overline{\mathit{x}}$ ± SD)
Ph6	BBCH 511	j. days	101 ± 4,5	101 ± 6	100 ± 7	101 ± 5
		week	14.5 ± 0.7	14.5 ± 0.8	14.3 ± 1.0	14.5 ± 0.8
Ph7	BBCH 512	J. days	111 ± 6	114 ± 6	111 ± 7	113 ± 7
		week	15.9 ± 0.7	16.2 ± 0123.7	15.9 ± 0.9	16.1 ± 0.9
Ph8	BBCH 62	J. days	121 ± 7	123 ± 5	120 ± 8	126 ± 6
		week	17.3 ± 0.9	17.5 ± 0.7	17.1 ± 1.1	17.8 ± 0.9
Ph9	BBCH 652	J. days	135 ± 5	135 ± 5	135 ± 6	135 ± 7
		week	19.2 ± 0.8	19.3 ± 0.7	19.2 ± 0.9	19.3 ± 0.9
Ph10	BBCH 671	J. days	145 ± 6	147 ± 5	144 ± 4	147 ± 7
		week	20.7 ± 0.8	20.5 ± 0.8	20.6 ± 0.6	21.1 ± 0.9
Ph 11	BBCH 69	j. days	156 ± 7	157 ± 6	158 ± 8	161 ± 8
		week	22.2 ± 0.9	22.3 ± 0.8	22.4 ± 1.0	22.8 ± 1.1
Ph 12	BBCH 79	J. days	198 ± 10	202 ± 15	200 ± 17	209 ± 17
		week	28.4 ± 1.4	29.1 ± 2.2	28.8 ± 2.6	30.1 ± 2.5
Ph 13	BBCH 89	j. days	238 ± 19	245 ± 12	235 ± 18	257 ± 10
		week	34.6 ± 2.6	35.4 ± 2.0	33.8 ± 2.7	37.1 ± 1.3

shows the results of analysis of the dates of occurrence of the individual phenological phases depending on the form of cover where the observed trees grow. The average period of the initial appearance of phenological phases Ph1 to Ph3 (BBCH: 07, 11, 19) were similar, irrespective of the form of coverage in the area within which they were observed. Particularly noteworthy is phase Ph4 (BBCH 93), which is characterized by a considerable variability, ranging from 2 to almost four weeks. depending on the form of land cover. The phenophases of trees growing in green areas and by reservoirs and watercourses were characterized by a lower variability in their frequency compared to the variability of the phenophases of trees growing in the vicinity of high-rise areas and along communication routes, for which this variability was more than one week. Moreover, in trees growing along the streets, the beginning of leaf fall occurred 2 weeks earlier than in trees growing near reservoirs and watercourses and with high-rise buildings. Even greater differences were noted in relation to trees growing in green areas—over 3 weeks. In the case of flowering, no clear differences were noted between the phenophases of trees growing depending on the form of land cover, within limits and the same was true for their variability.

The analysis of the duration of phenological phases, taking into account the form of land cover on which the observed specimens grow, showed that trees growing along communication areas have a shorter vegetative period compared to trees growing in other areas (

Table 7. Duration of vegetative phases (Ph1–Ph5) depending on the form of land cover (in weeks).

Green Spaces		Ph1	Ph2	Ph3	Ph4	Ph5	Street Areas		Ph1	Ph2	Ph3	Ph4	Ph5
	Ph1		-	-	-	-		Ph1		-	-	-	-
	Ph2	1.2		-	-	-		Ph2	1.0		-	-	-
	Ph3	4.6	3.4		-	-		Ph3	4.3	3.3		-	-
	Ph4	26.2	25.0	21.6		-		Ph4	23.1	22.1	18.8		-
	Ph5	32.2	31.0	27.6	6.0			Ph5	31.1	30.3	27.0	8.2
High-rise Building Areas		Ph1	Ph2	Ph3	Ph4	Ph5	Water Areas		Ph1	Ph2	Ph3	Ph4	Ph5
	Ph1		-	-	-	-		Ph1		-	-	-	-
	Ph2	1.2		-	-	-		Ph2	1.3		-	-	-
	Ph3	4.3	3.1		-	-		Ph3	4.6	3.3		-	-
	Ph4	25.4	24.2	21.1		-		Ph4	25.2	23.9	20.6		-
	Ph5	32.8	31.6	28.5	7.4			Ph5	32.1	30.8	27.5	6.9

Ph1-BBCH 07; Ph2-BBCH 11; Ph3-BBCH 19; Ph4-BBCH; Ph5-BBCH.

). This difference ranged from 1 week in comparison to the areas located by the reservoirs and watercourses to almost 2 weeks for trees growing in the vicinity of high-rise buildings. The leaves remained the longest on trees growing in the vicinity of tall buildings, where the vegetation lasted more than 1.5 weeks longer than in the streets.

Based on the frequency analysis (Figure 4), it was shown that trees growing along communication routes entered the growing season the latest, that is, in the 12th week of the year—during this time, the Ph1 phase was recorded in only 17% of specimens. In the same week, it was observed in approx. 50% of specimens growing in green areas, by water reservoirs and by tall buildings. Ph4 phase was the earliest observed on trees growing along streets. On the other hand, the longest leaves remained on trees growing in green areas and among tall buildings. Moreover, the Ph8 phase was observed at the latest on trees growing near water reservoirs and the Ph10 phase most often on trees growing along communication routes.

3.3. Form of Land Cover and Distance and Their Influence on Phenology

Based on the averaged dates of the beginning of the phenological phases, it was found that, regardless of the form of land cover, the Ph1 phase was observed at the latest on trees growing in zone Z4 (

Table 8. Average phenological data ($\overline{x}$) and variability (±SD) in individual groups of land cover forms. taking into account the distance from the center [in weeks and Julian days].

No. of Phenological Phase	BBCH Code		Street Areas				Green Spaces
			Z1	Z2	Z3	Z4	Z1	Z2	Z3	Z4
Ph1	BBCH 07	j. days	89 ± 3	87 ± 4	89 ± 1	94 ± 10	85 ± 3	86 ± 4	90 ± 7	90 ± 5
		week	12.8 ± 0.4	12.5 ± 0.6	13.0 ± 0.0	13.6 ± 1.3	12.3 ± 0.5	12.4 ± 0.5	13.0 ± 1.0	13.0 ± 0.7
Ph2	BBCH 11	j. days	95 ± 7	93 ± 5	98 ± 1	101 ± 6	93 ± 4	96 ± 4	100 ± 6	99 ± 3
		week	13.8 ± 0.8	13.8 ± 0.5	14.0 ± 0.0	14.3 ± 0.8	13.4 ± 0.5	13.8 ± 0.4	14.5 ± 0.8	14.1 ± 0.4
Ph3	BBCH 19	j. days	120 ± 5	119 ± 6	123 ± 8	123 ± 6	117 ± 7	122 ± 8	124 ± 8	124 ± 7
		week	17.0 ± 0.7	16.8 ± 0.8	17.5 ± 1.2	17.6 ± 1.0	16.6 ± 0.9	17.3 ± 1.0	17.8 ± 1.2	17.7 ± 1.1
Ph4	BBCH 93	j. days	250 ± 29	243 ± 12	251 ± 37	259 ± 16	273 ± 15	271 ± 21	275 ± 20	265 ± 17
		week	36.0 ± 3.9	35.0 ± 1.9	36.1 ± 5.2	37.1 ± 2.3	39.1 ± 2.0	39.0 ± 2.8	39.5 ± 2.6	38.0 ± 2.4
Ph5	BBCH 97	j. days	310 ± 10	303 ± 13	311 ± 11	312 ± 6	323 ± 8	313 ± 16	309 ± 11	308 ± 11
		week	44.5 ± 1.2	43.5 ± 1.9	44.5 ± 1.4	44.7 ± 0.8	46.3 ± 1.0	44.8 ± 2.0	44.2 ± 1.3	44.0 ± 1.2
Ph6	BBCH 511	j. days	97 ± 6	96 ± 6	104 ± 4	104 ± 5	100 ± 5	98 ± 1	103 ± 6	104 ± 4
		week	14.0 ± 0.7	13.8 ± 0.8	14.9 ± 0.6	14.9 ± 0.7	14.4 ± 0.7	14.0 ± 0.0	14.7 ± 0.8	14.9 ± 0.7
Ph7	BBCH 512	j. days	110 ± 6	111 ± 3	116 ± 6	116 ± 4	108 ± 5	111 ± 8	113 ± 3	114 ± 6
		week	15.8 ± 0.8	15.8 ± 0.4	16.5 ± 0.8	16.5 ± 0.5	15.5 ± 0.8	15.8 ± 1.0	16.2 ± 0.5	16.2 ± 0.7
Ph8	BBCH 62	j. days	121 ± 6	120 ± 5	124 ± 4	126 ± 4	115 ± 4	119 ± 7	126 ± 4	127±4
		week	17.2 ± 0.8	17.0 ± 0.6	17.6 ± 0.5	17.9 ± 0.7	16.4 ± 0.5	17.0 ± 1.0	17.8 ± 0.5	18.0 ± 0.5
Ph9	BBCH 652	j. days	130 ± 3	132 ± 3	137 ± 4	138 ± 4	129 ± 3	133 ± 4	138 ± 4	139 ± 3
		week	18.6 ± 0.6	18.8 ± 0.4	19.6 ± 0.5	19.7 ± 0.5	18.4 ± 0.5	19.0 ± 0.6	19.7 ± 0.5	19.9 ± 0.4
Ph10	BBCH 671	j. days	141 ± 9	140 ± 4	145 ± 3	145 ± 3	141 ± 6	144 ± 3	147 ± 1	148 ± 7
		week	20.2 ± 1.3	20.2 ± 0.8	20.8 ± 0.5	20.7 ± 0.5	20.1 ± 1.0	20.7 ± 0.5	21.0 ± 0.0	21.1 ± 0.9
Ph11	BBCH 69	j. days	158 ± 6	156 ± 7	157 ± 5	157 ± 6	154 ± 6	154 ± 8	157 ± 4	159 ± 8
		week	22.4 ± 0.9	22.2 ± 1.0	22.4 ± 0.7	22.3 ± 0.8	22 ± 0.8	21.8 ± 1.0	22.3 ± 0.5	22.7 ± 1.1
No. of Phenological Phase	BBCH code		High-rise Building Areas				Water Areas
			Z1	Z2	Z3	Z4	Z1	Z2	Z3	Z4
Ph1	BBCH 07	j. days	86 ± 4	87 ± 6	86 ± 4	89 ± 6	83 ± 0	88 ± 9	92 ± 6	94 ± 5
		week	12.4 ± 0.5	12.5 ± 0.8	12.5 ± 0.6	13.0 ± 0.8	12.0 ± 0	12.7 ± 1.2	13.2 ± 0.8	13.5 ± 0.7
Ph2	BBCH 11	j. days	95 ± 4	94 ± 5	95 ± 8	100 ± 3	96 ± 6	101 ± 4	101 ± 4	101 ± 4
		week	13.7 ± 0.5	13.8 ± 0.6	13.5 ± 1.0	14.2 ± 0.4	13.7 ± 0.6	14.3 ± 0.6	14.2 ± 0.4	14.3 ± 0.6
Ph3	BBCH 19	j. days	118 ± 4	117 ± 8	118 ± 13	124 ± 4	122 ± 4	119 ± 8	124 ± 8	122 ± 4
		week	16.7 ± 0.5	16.7 ± 1.0	16.8 ± 1.8	17.6 ± 0.5	17.3 ± 0.6	17.0 ± 1.0	17.8 ± 1.3	17.3 ± 0.6
Ph4	BBCH 93	j. days	260 ± 30	266 ± 20	276 ± 18	261 ± 17	280 ± 0	272 ± 0	255 ± 22	266 ± 24
		week	37.4 ± 4.2	38.2 ± 2.7	39 ± 2.3	37.4 ± 2.2	40.0 ± 0.0	39.0 ± 0.0	36.8 ± 3.0	37.0 ± 3.5
Ph5	BBCH 97	j. days	316 ± 10	318 ± 11	319 ± 12	313 ± 9	319 ± 8	308 ± 14	309 ± 14	315 ± 3
		week	45.3 ± 1.4	45.7 ± 1.6	45.8 ± 1.8	45.0 ± 1.4	46.3 ± 1.2	44.3 ± 2.3	44.4 ± 1.9	45.0 ± 0.0
Ph6	BBCH 511	j. days	99 ± 6	101 ± 9	95 ± 7	104 ± 8	96 ± 6	101 ± 3,5	105 ± 5	105 ± 5
		week	14.3 ± 0.8	14.5 ± 1.2	13.6 ± 0.9	15.0 ± 1.0	13.7 ± 0.6	14.3 ± 0.6	15.0 ± 0.7	14.7 ± 0.6
Ph7	BBCH 512	j. days	111 ± 6	109 ± 9	106 ± 6	117 ± 5	107 ± 4	112 ± 8,0	115 ± 5	118 ± 7
		week	15.9 ± 0.9	15.7 ± 1.2	15.4 ± 0.9	16.6 ± 0.5	15.3 ± 0.6	16.0 ± 1.0	16.4 ± 0.5	16.7 ± 1.2
Ph8	BBCH 62	j. days	120 ± 6	120 ± 9	117 ± 13	126 ± 3	122 ± 4	124 ± 6	127 ± 5	130 ± 7
		week	17.0 ± 0.8	17.0 ± 1.2	16.6 ± 1.8	17.8 ± 0.4	17.3 ± 0.6	17.7 ± 1.2	18.0 ± 0.7	18.3 ± 1.2
Ph9	BBCH 652	j. days	134 ± 6	134 ± 8	137 ± 6	137 ± 5	131 ± 0	131 ± 7	136 ± 9	142 ± 7
		week	19.0 ± 0.8	19.0 ± 1.1	19.4 ± 0.9	19.6 ± 0.5	19.0 ± 0.0	18.7 ± 1.2	19.4 ± 1.1	20.0 ± 1.0
Ph10	BBCH 671	j. days	145 ± 4	145 ± 3	142 ± 6	142 ± 4	145 ± 0	149 ± 12	150 ± 7	145 ± 4
		week	20.7 ± 0.5	20.8 ± 0.4	20.4 ± 0.9	20.4 ± 0.5	21.0 ± 0.0	21.3 ± 1.5	21.4 ± 0.9	20.5 ± 0.7
Ph11	BBCH 69	j. days	157 ± 4	163 ± 11	154 ± 8	155 ± 7	162 ± 0	161 ± 16	162 ± 9	156 ± 4
		week	22.4 ± 0.5	23.2 ± 1.4	22.0 ± 1.0	22.2 ± 0.9	23.0 ± 0.0	23.0 ± 2.0	23.0 ± 1.2	22.3 ± 0.6

). The Ph1 phase, regardless of the zone, was first observed on trees growing near high-rise buildings. It was most clearly visible in the Z4 zone. Similar results were obtained for trees growing in green areas. The Ph1 phase is observed the least in trees growing along communication routes compared with areas of different forms of coverage, especially in zone Z4. Similar results were obtained for trees growing near watercourses and reservoirs, however, less variability of phenophases was observed here.

Ph4 was observed on average in weeks 36–37 along communication routes and in green areas in the 39th week of the year, regardless of the distance of the trees from the center (Table 8). The variability of the Ph4 phase was greater in the areas of communication and the differences ranged from 2 to even 5 weeks for trees growing in the Z3 zone. In extreme cases, for trees growing along communication routes, the fall of leaves was noted in week 29 in zone Z1 and in week 25 in zone Z3. In trees growing in green areas, the variation in the appearance of the phase was smaller and ranged from 2 to 3 weeks, depending on their location from the city center In the case of high-rise buildings, the Ph4 phase in zone Z1 and Z4 was, on average, in the first half of the 37th week, while in trees growing in zone Z4, the variability of its occurrence was 2 weeks and in zone Z1, as much as 4 weeks. In the case of trees growing at reservoirs and watercourses, the beginning of leaf fall occurred on average in the 40th week in zone Z1.

The leaves lasted longer on trees growing near high-rise buildings and in green areas when compared to trees growing near communication routes (Table 8). The difference was that trees growing near tall buildings were characterized by a greater phase variation compared to trees growing in green areas. In green areas at a distance of up to 1 km (Z1), this phase lasted approx. 1.5 weeks longer compared to trees growing in green areas in other zones.

It can be seen that in trees growing along communication routes in zones Z3 and Z4, the Ph7 phase occurred on average about a week later than in zones Z1 and Z2. Similar observations occurred for high-rise buildings but the differences in this case were half a week. In green areas, the Ph7 phase occurred on average half a week later for each subsequent zone.

4. Discussion

Our study presents the results of one vegetation period, such as in Schmidlin [68], Zhang et al. [28] or Jochner et al. [30]; however, as shown by Zipper et al. [27], the magnitude of changes in the phenology associated with UHI is strongly determined by the prevailing weather conditions, which may lead to generalization of the results. Therefore, it is necessary to continue the observations taking into account air temperature and humidity, precipitation or air relative humidity. On the other hand, Zipper et al. [27] showed that despite some differences in the results from single years of observation, the results taking into account spatial patterns may be the same over the years. Similarly, Buyantuyev and Wu [12] showed that phenological diversity results to a large extent from the degree of urbanization and is not synchronized with climatic variability. Ding et al. [38] suggests that urbanization, through surface warming, compounds the effect of climate change on vegetation phenology.

The acceleration of the initial phases and the extension of the growing season in the city center, which we have seen in Wrocław, is consistent with the results obtained for Munich in Germany [57], for Campinas in Brazil [30], for cities in Yangtze River Delta in China [38] or for Madison in the USA [27]. In our studies, based on average values, it was observed that the growing season for horse chestnut in the center of the city lasted an average of two weeks longer than in peripheral areas situated more than 5 km from the center. Zipper et al. [27] observed, on the basis of studies using remote sensing, an extension of the growing season by 10–25 days and on the basis of air temperatures, by approx. 8–11 days. Zipper et al. [27], who based their research on remote sensing and assessment of the degree of greening, suggest that the acceleration of the growing season and its extension in the city center compared to peripheral areas may be related to species diversity. According to these authors, the introduced winter-hardy species are often used in the city center, whereas the native, deciduous species appear in rural areas. The results obtained in this study on the basis of the observation of the horse chestnut confirm the spatial relationship without any relation to species diversity and are consistent with the results of other researchers around the world [44]. However, it was noticed that the extension of the growing season is related to the earlier development of plants in the spring (starting phases) in the center zone compared to the peripheral areas, with a similar end time to the growing season. The premature defoliation of horse chestnut trees is also influenced by Cameraria ohridella and the authors’ observations show that in the city center, where leaves fell from all zones the latest, the degree of infection with Cameraria ohridella is lower than in the peripheries. This may be related to the greater sterility of central city areas compared to the peripheries, where the leaves, in which the larvae of pests spend the winter, are more frequently and systematically removed.

Jochner et al. [30] showed that temperate zone plants in cities bloom earlier than plants in rural areas due to higher local temperatures, this was especially noticeable for the blooming phenophases of warty birch in Munich. This is also confirmed by the results presented in this study for trees growing in zones up to 2 km from the city center, which bloomed earlier than trees located 5 km from the city center The influence of air temperature on the flowering rate is also visible in the waterside areas; naturally cooler with higher humidity and lower water vapor deficit in the air, where flowering was observed at the latest phase in relation to other forms of land cover.

Li et al. [34] and Wohlfahrt et al. [69], based on their work, believe that the effects of UHI (measured by the daily earth surface temperature) alone cannot explain the overall impact of the degree of urbanization on plant phenology. This suggests that urbanization also influences plant phenology through other mechanisms, which is why the research also considered the form of land use in which the specimens are grown. On the basis of phenological observations carried out in Wrocław, the results obtained for the assessment of the impact of individual types of terrain were statistically confirmed only for areas located near communication routes and green areas. However, the analysis of the timing of the occurrence of individual phenological phases shows that the course of phenophases for green areas and areas near reservoirs and watercourses (although the work of Schatz and Kucharik [70] showed that the zone of water reservoir influence on temperature is relatively small—it has the strongest impact in the zone up to 100 m), in relation to built-up areas and surrounded by impermeable surfaces, is characterized by less variability.

Despite the initially similar development of trees in all the considered forms of land cover, a delay in the appearance of the final phases (leaf fall) for green areas is noticeable compared to street areas. The results of Zipper et al. [27] also showed intermediate results for the start and end of the growing season based on air temperatures for park areas versus urban and rural areas. As suggested by Yu and Hien [71], Feyisa et al. [72] and Zipper [27], green areas and urban parks are subject to both the urban heat island effect, which raises the temperature in relation to the rural environment and the cool island effect, which lowers the temperature in relation to their urban surroundings. Green areas are characterized by lower air temperature fluctuations during the day and less heating of the ground surface due to shading.

The phenological development of plants is related not only to temperatures—it is influenced by the growing conditions of the tree, the individual size and age of the tree, the tree vitality and water stress [73,74,75,76]. Urban trees often experience the negative effects of excessive soil compaction [77] and too little growth space with limited availability of water and nutrients [78], and, as a consequence, it affects the life processes of plants. Sobolewski and Chohura [79] showed that soils in road lanes in Wrocław are characterized by a low level of nitrogen available for plants and high levels of Ca, Na and Cl, which in turn has an impact on the nutritional status of trees. Łukasiewicz and Oleksy [80] showed that the size of the soil surface around horse chestnut trees directly influences the differentiation of average temperatures (including maximum and minimum temperatures), humidity and insufficient air humidity as well as the intensity of transpiration. The authors also indicate that in an urbanized environment, a sufficiently large, unpaved soil surface affects, among other things, the length of the foliage phase, which our research supports. These aspects may explain our observation of extreme cases, when the process of defoliation of leaves of trees began already in the 29th week of the year. Jochner et al. [53] showed that the increase in the concentration of O3, NO2, NOx and PM, significantly delayed the phenological phases of warty birch, horse chestnut and common hazel, these relationships were more noticeable in the city center than in non-urban areas. However, Borowski and Pstrągowska [81] drew attention to the delay of the cracking of lime buds growing in road lanes and thus delay in phenological development as a result of their damage by salt aerosol depositing on their surface during winters. This study may explain why, in our observations of trees growing along the routes, developed later. Chen et al. [82] have shown, however, that heating of the surface of concrete/impermeable surfaces may affect the temperature rise of the soil, while the increased soil temperature accelerates the breakage of leaf buds in Fraxinus chinensis. Shashua-Bar et al. [83] showed that reducing traffic by half reduces the ambient temperature and therefore intensive traffic increases the local temperature, which may be an additional factor supporting faster defoliation of trees in road lanes. Some studies suggest that elevated CO2 levels in the city may delay the coloration and aging of tree leaves in autumn [84]. Similar observations were made by Reference [12] who indicate that urban ban lighting may extend the defoliation process over time. The aforementioned processes may explain the complexity of the impact of numerous independent factors influencing the phenology of plants in urban areas, which would explain the observations concerning the extended vegetation period in the city center as well as the shortened vegetation period in road lanes.

5. Conclusions

• Patterns of the effects of distance and surroundings on the phenology of the horse chestnut have been documented mainly for the initial and final stages of foliage and initial stages of flowering.
• The surroundings and the distance from the city center affect the phenology of trees of the studied species in urbanized areas, which results in the delay and acceleration of individual phenological phases, however, due to the heterogeneous structure of urban areas and its geometry, research in this area is difficult and laborious.
• The results obtained on the basis of phenological observations carried out in 2017 in Wrocław confirmed the extension of the period of vegetation in the city center in relation to its peripheries.
• Trees growing in road lanes entered the vegetation period later and defoliated faster, which confirms the negative impact of street conditions on the development of trees in urban space. Thus, the growing season in road lanes is shorter and due to the 1-year observation period, it is justified to conduct further observations.
• The article may become the next step in improving the methodology of carrying out phenological observations in urban areas, taking into account its characteristic heterogeneous spatial structure.
• Research in this area should be continued, the results of several years of observation may enrich knowledge on the impact of local climate and urbanization on urban trees.