Evaluating the Effects of Solar Radiation Parameter on Radial Growth of Quercus castaneifolia in Astara Forests

Document Type : Research Paper

Authors

1 M. Sc Student of Forestry, Department of Forestry, Faculty of Natural Resources, University of Guilan, Iran,

2 Assistant Prof. of Forestry, Department of Forestry, Faculty of Natural Resources, University of Guilan, Iran,

3 Assistant Prof. of Forestry, Department of Forestry, Faculty of Natural Resources, University of Guilan, Iran

4 M. Sc of Forestry, Natural Resources and Watershed Office of Astara, Astara, Iran

Abstract

 
Introduction
Climate change happens due to abnormal changes of climate within the earth’s atmosphere and their consequences. One of the most significant effects of climate change is the irreversible damage to some floral species and forest ecosystems. Tree species reflect the impact of climate changes on their ring width. Generally, tree rings vary in size each year depending upon the environmental conditions or climate variables that the tree experiences. In fact, tree rings are severely dependent on the changes of climate variables. It is considered a basis for “dendrochronology” which is the scientific method of dating based on the analysis of patterns of tree rings or investigation of climate variables effects on tree ring width. Many national and international studies have been conducted on dendrochronology. However, the national researches investigated the effects of temperature and rainfall changes on radial growth of trees. Unfortunately, due to lack of long-term solar radiation data in the most of meteorological stations in Iran, the effect of this parameter on the radial growth of trees has not been studied so far. Meanwhile the solar radiation has a significant effect on the width of tree rings-especially in tolerant shaded species like oak. One of the most important species of trees in Iran is the Oak tree (Quercus castaneifolia), due to its being spread in different areas of the country and its high economic and environmental value. Unfortunately, in recent years, because of climate changes and droughts, and also overcutting of Quercus castaneifolia for wood and live-stokes food supply, this precious species has been subjected to serious threats. In this regard, the role of climate in addition to improper management is significant. To protect Quercus castaneifolia, the first and most important step is the scientific planning of forest management, through knowing the effective parameters of climate change on the growth and physiology of the trees. Therefore, implementation of more research on the oak species and utilizing the results is essential for their protection.    
By considering the above mentioned facts, to solve the problem related the lack of solar radiation data, in this study, an appropriate methodology was introduced based on empirical formulas for calculating the solar radiation. Thereafter, the incoming solar radiation in the Astara Forests was calculated. In the next step, by using seven discs harvested from Quercus castaneifolia trees, the chronology of this species for each disc in two perpendicular directions was obtained by using LINTAB tool coupled to TSAPWin software. Finally, the relationship between tree ring widths and climate variables was determined.
 
 
Materials and Methods
In this research the seven discs were harvested from Quercus castaneifolia trees with mean tree ages of 35 to 78 years in the Astara Forests located in north of Iran. In addition, the climate variables were collected from the synoptic meteorological station of Astara. However, due to financial, technical or institutional limitations, the solar radiation data are absent, incomplete or inaccessible in most areas of the world especially in the developing countries such as Iran. This seriously hinders the progress of forestry researches such as chronology studies that require solar radiation as a key driving input. Therefore, various methods have been explored in order to estimate, with reasonable accuracy, the solar radiation from other available meteorological data. One kind of widely used method is based on empirical relations between solar radiations and commonly measured meteorological variables. Therefore, in this research, Angstrom-Prescott model (Eq. (1)) was selected to estimate the monthly and yearly global solar irradiation (Rs) in the Astra Forests.





(1)

 




In the next step, the chronology of each disc in two perpendicular directions was obtained by using LINTAB tool coupled to TSAPWin software. To evaluate the obtained chronology for each disc, the Gleichläufigkeit (GLK), Crossdate Index (CDI), and Signature GLK (GSL) were used.
 
Results
According to published results on determination of a and b parameters of Angstrom-Prescott model for different regions of Iran, 0.404 and 0.204 were selected for Astra Forests district, respectively. Afterwards, using recorded meteorological parameters in Astara Synoptic Station, the monthly and annual global solar irradiation were estimated for Astra Forests during 1985 to 2005 (Fig. 1).
 
 
Fig. 1: Annual and Monthly Average of Rs
 
In the next step, the chronology of species for each disc in two perpendicular directions indicated that statistical indexes had appropriate values. Findings showed that the average of chronology for each disc derived from two vertical directions was significant. In the other words, three useful parameters for evaluating the chronology’s quality of all seven discs i.e., GLK, CDI, and GSL were more than 73, 46, and 99.9%, respectively. Thereafter, the average sizes of two perpendicular directions for each of the seven discs were calculated and the chronology of the average values was carried out. Only four of the discs showed proper results according to their indices. Using the chronology of the four discs, the regional chronology of Quercus castaneifolia trees in Astara Forests was calculated (Fig. 2). Ultimately, a statistical relation was determined between the Rs and the chronology of these trees (Fig.3).
 
 
Fig. 2: Regional chronology of Quercus castaneifolia trees in Astra Forests
 
 
Fig. 3: Quercus castaneifolia trees ring widths vs Rs
 
Discussion and Conclusion
Quercus castaneifolia tree ring widths vary with Rs by a second order polynomial function. The R value of this function (-0.71) is proper, which is an indicator of a strong relationship between Rs and Quercus castaneifolia tree ring widths. The negative value of R shows an inverse relationship, an expected fact which obviously reflects the shade intolerant quality of oak species. According to the similarity of temperature and Rs and also to the previous studies on the effect of temperature on tree ring widths, which resulted in negative R values, it can be concluded that the findings of the present research are reliable and justified

Keywords

Main Subjects


 
ارسلانی، م.، عزیزی، ق.، خوش‌اخلاق، ف. 1391. بازسازی تغییرات دمای حداکثر استان کرمانشاه با استفاده از حلقه‌های درختی، جغرافیا و مخاطرات محیطی، شمارۀ 1، صفحات 97- 110.
بالاپور، ش. 1386. بررسی تأثیر فاکتورهای مهم اقلیمی (بارندگی و دما و ترکیب آن‌ها) روی حلقه‌های رویشی گونه‌های راش و بلندمازو، پایان‌نامۀ کارشناسی ارشد، دانشگاه مازندران، 140 صفحه.
بالاپور، ش.، جلیلوند، ح.، رائینی، م.، اسدپور، ح. 1389. رابطۀ حلقه‌های رویشی راش با برخی از متغیرهای اقلیمی در جنگل آموزشی- پژوهشی دانشکدۀ منابع طبیعی ساری (دارابکلا)، پژوهش‌های آبخیزداری، شمارۀ 88، صفحات 1- 10.
بالاپور، ش.، کاظمی، س. 1391. مطالعۀ اثر متغیرهای اقلیمی (دما و بارندگی) روی رویش سالیانۀ گونۀ آزاد (Zelkova carpinifolia)، تحقیقات علوم چوب و کاغذ ایران، جلد 27، شمارۀ 1، صفحات 69- 80.
پورسرتیپ، ل. 1385. مقایسۀ رویش شعاعی درختان ارس (Juniperus polycarpos) و اوری (Quercus macranthera) در دو دامنۀ شمال و جنوب البرز در منطقۀ چهارباغ گرگان، پایان‌نامۀ ارشد دانشکدۀ منابع طبیعی دانشگاه تهران، 90 صفحه.
پورطهماسی، ک.، پارساپژوه، د.، مروی مهاجر، م.ر.، علی‌احمد کروری، س. 1387. ارزیابی رویش شعاعی درختان ارس (Juniperus polycarpos C.Koch) در سه رویشگاه ایران با استفاده از دانش گاه‌شناسی درختی، تحقیقات جنگل و صنوبر ایران، شمارۀ 2، صفحات 327- 342.
پورطهماسی، ک.، پورسرتیپ، ل.، براونینگ، آ.، پارساپژوه، د. 1388. ارزیابی رویش شعاعی درختان ارس (Juniperus polycarpos) و اوری (Quercus macranthera) در دو دامنۀ شمال و جنوب البرز در منطقۀ چهار باغ گرگان، جنگل و فرآورده‌های چوب (منابع طبیعی ایران)، جلد 62، شمارۀ 2، صفحات 159- 169.
جعفری، م. 1387. تحقیق و تحلیل عوامل تغییر اقلیم طی پنجاه سال گذشته در جنگل‌های منطقۀ خزری، تحقیقات جنگل و صنوبر ایران، شمارۀ 2، صفحات 314- 326.
صفاری، م.، ایوبی، ا.، بخشی، ر.، کیایی، م. 1390. بررسی اثر متغیرهای اقلیمی بر حلقه‌های رویشی چوب گونه بلوط (Quercus castaneaefolia) (مطالعۀ موردی: طرح تلیم رود تنکابن)، فصلنامۀ علوم و فنون منابع طبیعی، شمارۀ 2، صفحات 106- 113.
عزیزی، ق.، ارسلانی، م.، ارسلانی، ع.، صفایی‌راد، ر. 1391. بازسازی دمای بیشینۀ بهار- تابستان در یال غربی زاگرس میانی با استفاده از یک گاه‌شناسی منطقه‌ای (1750- 2010)، جغرافیا و مخاطرات محیطی، شمارۀ 4، صفحات 51- 64.
کرم‌زاده، س.، پوربابایی، ح.، ترکمن، ج. 1390. اقلیم‌شناسی درختی (Dendroclimatology) بلندمازو در منطقۀ سراوان گیلان، تحقیقات جنگل و صنوبر ایران، شمارۀ 19، صفحات 15- 26.
معینی، س.، جوادی، ش.، کوکبی، م.، دهقان منشادی، م. 1389. برآورد تابش خورشیدی در ایران با استفاده از یک مدل بهینه، نشریۀ انرژی ایران، شمارۀ 2، صفحات 1- 10.
Akkemik, Ü., Nasibe, D. and Aliye, A. 2005. A preliminary reconstruction (A.D. 1635–2000) of spring precipitation using oak tree rings in the western Black Sea region of Turkey. International Journal of Biometeorology, 49(5): 297-302.
Bao, G., Song, H., Cai, Q. and Sun, J. 2009. Precipitation reconstruction from Hailar pine (Pinus sylvestris var. mongolica) tree rings in the Hailar region, Inner Mongolia, China back to 1865 AD.  Palaeogeography, Palaeoclimatology, Palaeoecology, 282(1-4): 81-87.
Cooper, P.I. 1969. The absorption of solar radiation in solar stills. Solar Energy, 12(B): 333-346.
Cooper, R.J., Melvin, T.M., Tyers, I., Wilson, R.J.S. and Briffa, K.R. 2013. A tree-ring reconstruction of East Anglian (UK) hydroclimate variability over the last millennium. Climate Dynamics, 40(3-4): 1019-1039.
Duffie, J.A. and Beckman, W.A. 1992. Solar Energy Engineering. John Wiley, USA, 324p.
Gervais, B. 2006. A three-century record of precipitation and blue oak recruitment from the Tehachapi Mountains, Southern California, USA. Dendrochronologia, 24(1): 29-37.
Li, Z.S., Zhang, Q.B. and Ma, K. 2012. Tree-ring reconstruction of summer temperature for A.D. 1475–2003 in the central Hengduan Mountains, Northwestern Yunnan, China. Climatic Change, 110(1-2): 455-467.
Özçelik, R., Diamantopoulou, M.J., Crecente-Campo, F. and Eler, U. 2013. Estimating Crimean juniper tree height using nonlinear regression and artificial neural network models. Forest Ecology and Management, 306: 52-60.
Schweingruber, F.H. 1988. Tree Rings: Basics and Applications of Dendrochronology. Kluwer Academic Publishers, Dordrecht, Netherlands. 276p.