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Unveiling the Dendroclimatic Potential of Blue Pine (Pinus wallichiana) Growing in Shangla, Khyber Pakhtunkhwa

Unveiling the Dendroclimatic Potential of Blue Pine (Pinus wallichiana) Growing in Shangla, Khyber Pakhtunkhwa

Tanvir Hussain*, Zahid Rauf, Mansoor Ali Khan and Khalid Hussain 

Pakistan Forest Institute, Peshawar -25130, Khyber Pakhtunkhwa, Pakistan.

 
*Correspondence | Tanvir Hussain, Pakistan Forest Institute, Peshawar -25130, Khyber Pakhtunkhwa, Pakistan; Email: [email protected] 

Figure 1:

Shangla meteorological data’s Climatogram for the Years 1921–2021.

Table 2:

Tree ring chronology from Shangla Forest Area using Cofecha statistics.

Figure 2:

The Shangla forest area, Swat, regional tree ring width chronology from 1921 to 2021. The sample depth is shown by the gray region.

Figure 4:

Analysis of correlation function for Kail at Shangla; correlation coefficient (r) between monthly meteorological variable and TRW for the current year (capital letters) and the previous year (lower case). Stick bars represent statistically significant associations (p<0.05) (Sohar et al., 2017). The common era (1921-2021) was used to compute correlations between June of the year before tree-ring growth and October of the current growth year (Ahmed et al., 2010).

Figure 3:

Blue pine growing in Shangla, KPK, from 1921 to 2021: Positive and negative pointer and event years.

Pakistan Journal of Forestry

June

Vol. 74, Iss. 1

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