=Paper=
{{Paper
|id=Vol-2761/HAICTA_2020_paper63
|storemode=property
|title=Seasonal Air Temperature Variability and Trends in a Mountainous Forest Ecosystem of Central Greece
|pdfUrl=https://ceur-ws.org/Vol-2761/HAICTA_2020_paper63.pdf
|volume=Vol-2761
|authors=Stefanos Stefanidis,Chrysoula Chatzichristaki,Panagiotis Stefanidis
|dblpUrl=https://dblp.org/rec/conf/haicta/StefanidisCS20
}}
==Seasonal Air Temperature Variability and Trends in a Mountainous Forest Ecosystem of Central Greece==
https://ceur-ws.org/Vol-2761/HAICTA_2020_paper63.pdf
Seasonal Air Temperature Variability and Trends in a
Mountainous Forest Ecosystem of Central Greece
Stefanos Stefanidis1, Chrysoula Chatzichristaki2, Panagiotis Stefanidis2
1
School of Forestry and Natural Environment, Aristotle University of Thessaloniki,
University Campus 54124, PO Box 268, Thessaloniki, Greece; e-mail: ststefanid@gmail.com
2
School of Forestry and Natural Environment, Aristotle University of Thessaloniki,
University Campus 54124, PO Box 268, Thessaloniki, Greece
Abstract. During the last decades, a progressive increase of temperature in
Mediterranean region was recorded. This change effect both natural
ecosystems and human activities. In this study, the variability and trends of
mean air temperature in the University Forest of Pertouli (Central Pindus,
Greece) was evaluated. To this end, long-term (1961-2019) time series for air
temperature from a mountainous meteorological station were collected and
analyzed. The seasonal data were subjected to Mann-Kendall test to assess the
possible upward or downward statistical significant trends and in case of a
significant trend to detect approximately its time of occurrence. Additionally,
least square method was used to estimate the trend magnitude. The results
showed warming trends in all seasons which they found statistical significant.
Finally, the magnitude trend since 1961 (58 years period) is approximately +
1.4oC, +1.1 oC, +1.3 oC and 1.2 for the winter, autumn, spring and summer
mean air temperature.
Keywords: climate change; temperature; Mann-Kendall; least square method;
trend.
1 Introduction
Air temperature is an important climatic component and it is governed by many
factors, including incoming solar radiation, humidity and altitude. In addition, it
present seasonal and diurnal variations and highly influence hydrological cycle
(Mavromatis and Stathis, 2011, Myronidis et al., 2012, Myronidis et al., 2018),
tourism decision making (Endler and Matzarakis, 2011, Matzarakis and Nastos,
2011,) and vegetation distribution (Wason et al., 2017, Kamoutsis et al., 2018, Macek
et al., 2019).
Climatological studies showed that global average surface temperature increased
by about 0.85 °C between 1880 and 2012, while the current rate of warming over the
past 60 years (1951-2012) is 0.12 °C per decade (IPCC, 2013). The
Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report (IPCC,
436
2013) emphasizes that the Mediterranean basin is expected to become warmer and
dryer until the end of the 21th century, while future warming will possibly be larger
than the global mean (Giorgi and Lionello, 2008). Climate changes compounded with
trends of rural abandonment will highly influence natural ecosystems within the
Mediterranean basin. It is also reported that are likely to diminish forested areas that
will be replaced by shrub lands (Resco de Dios et al., 2007).
The trend analysis of air temperature time series indicated a positive trend in the
western Mediterranean and a negative trend in the eastern Mediterranean for the
period 1950-1990 (Sahsamanoglou and Makrogiannis, 1992, Parker et al., 1994).
Many papers have been published dealing with the temperatures trend analysis in
Greece. An overall cooling trend was detected in winter air temperature for the
period 1951-1993 (Proedrou, 1997). The same cooling trend was also noted for the
mean annual and summer values, although a reverse warming trend was detected
around the mid-1970s at several stations. Also, according to Feidas et al. (2004)
cooling trend was mentioned for winter, whereas warming signal detected in summer
for the period (1955-2001). In addition, a more recent research by Feidas (2017)
updated with the 12-year period 2002–2013 found that the warming signal detected
previously only in summer has now intensified and spread in other seasons. A
cooling trend was also found by Nastos et al. (2011) for mean annual air temperature
(1951-2007) in the wider region of Greece. A pronounced cooling trend from the
beginning of the 1950s up to the mid-1970s was exhibited. It then remained at low
levels until the beginning of the 1990s, and then increased up to 2000, when a
turning-point is clear although the temperature remained at high levels. Another
study conducted by Mamara et al. (2016), examining the mean air temperature
(1960-2004), highlighted a statistically significant negative trend during 1960–1976
and a positive one during 1977–2004.
However, there are limited studies analyzing seasonal trends considering data
from mountainous meteorological stations (Proutsos et al., 2010). This is due to
difficulties of installation and maintenance of meteorological instruments, especially
at the high altitude of the mountainous regions.
The object of this study is to analyze variability and detect trends in long term
(1961-2019) seasonal air temperature time-series based on data from a mountainous
meteorological station located in Central Greece.
2 Material and Methods
Observations of daily mean air temperature (oC) for the period 1961-2019 were
collected, from a mountainous meteorological station (1180 m.a.s.l) located in the
University Forest of Pertouli, over the mountainous range of Pindus (Central Greece)
(Fig.1). The rights for the management of Pertouli forest was assigned to the
Aristotle University of Thessaloniki in 1934 for educational and research purposes. It
covers an area of 3.290 ha and consists mainly of pure fir stands (Abies borisii-regis).
Moreover, the region has great environmental importance as belongs to the European
nature conservation network Natura 2000 according to the criteria of Directive
437
92/43/EEC and specifically includes the Site of Community Importance (SCI) with
code GR1440002, namely "Kerketio Oros (Koziakas)".
The data series are complete, i.e. have no missing values. Double mass method
and two parametric statistical tests (Student’s t and Chi-Square test) were applied so
as to adjust any heterogeneity of the temperature data, while the details of these
methods can be obtained from WMO (1986). The latter tests demonstrated that the
temperatures data were indeed homogeneous.
Fig. 1. Location map of the study area.
Trend analysis was performed on seasonal time scale. Therefore, time series of air
temperature were subjected to a non-parametric Mann-Kendall test, as it has been
proposed by Sneyers (1990) so as to detect any trend over the examined period. A
lengthy description of the methodology and its computation can be found in the
literature (e.g. Feidas et al., 2004 Myronidis et al., 2012). The sequential form of the
Mann–Kendall test, consisting of the application of the test to all the series starting
with the first term and ending with the ith term (and the reverse), was also used for a
progressive analysis of the series. In the absence of any trend, the obtained graphical
representation of the direct (ut) and the backward (ut') series with this method
produced curves that overlap several times. However, in the case of a significant
trend (5 % level |ut|>1.96), the intersection of the curves enabled one to detect
approximately its time of occurrence. Furthermore, trend magnitudes were computed
based on least square method.
438
3 Results
The air temperature in the University Forest of Pertouli varied greatly between
seasons as shown in the following figure (Fig.2). It is noteworthy that mean
temperature range is 17.1 oC, for the examined period (1961-2019). As depicted,
mean air temperature is equal to 0.8 oC (-1.7 oC to 3.4 oC) in winter, 9.9 oC (6.7 oC to
11.8 oC) in autumn, 7.7 oC (4.7 oC to 9.8 oC) in spring and 17.9 (15.3 to 20.2) in
summer.
Fig. 2. Seasonal variability of mean air temperature.
Regarding the results of the Mann- Kendall test, statistically significant (at the
95% level of significance) warming trends were detected on seasonal air
temperatures. The beginning of the change starts in the early of 1980s for winter, at
the end of 1990s for autumn and spring and in the early of 1990s for summer (Fig 3).
439
Fig. 3. Graphical representation of the series u(t) and the retrograde series u'(t) of the
sequential version of Mann-Kendall test in a) winter, b) autumn, c) spring and d) summer.
Moreover, the least square method was used to compute trend magnitude. It was
found that the magnitude of the trend is approximately + 1.4oC, +1.1 oC, +1.3 oC and
1.2 in winter, autumn, spring and summer mean air temperature respectively, since
1961.
Fig. 4. Trend analysis of air temperature time series in a) winter, b) autumn, c) spring and d)
summer.
440
4 Conclusions
In this study, variability and trends of seasonal air temperatures in the University
Forest of Pertouli (Central Greece) for the period 1961-2019 were analyzed. Trend
analysis was based on a combination of two statistical tests.
The mean air temperature presents great variability and ranges from 0.8 oC
(winter) to 17.9 oC (summer). The results of the Mann-Kendal test highlighted
statistically significant warming trends in all seasons. Also, it was found that mean
temperature non-stationarity starts to occur in the early of 1980s for winter, at the end
of 1990s for autumn and spring and in the early of 1990s for summer. The trends
magnitude of mean air temperature during the last 58 year, using least square
method, computed to + 1.4oC for winter +1.1 oC for autumn, +1.3 oC for spring and
1.2 for summer. The warming in the study area is higher than the average in Greece
(Feidas, 2017). Also, the future climate condition is expected to be warmer until the
end of the 21th century
To this end, water availability, forest growth and snow cover period will be highly
influenced. The effects are not only environmental but also economic, as the
reduction of snow cover period will result in limitation of the operational days of ski
center resort in the area.
Acknowledgments. This research is co-financed by Greece and the European Union
(European Social Fund-ESF) through the Operational Programme «Human
Resources Development, Education and Lifelong Learning 2014-2020» in the
context of the project “Assessment of soil loss in mountainous catchment using
modern technology under climate change” (MIS 5047924). Additionally, the authors
would like to express their thanks to the University Forest Administration and
Management Fund of the Aristotle University of Thessaloniki for providing the
temperature time series data.
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