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Dinesh R. BHUJU Chief, Faculty of Science Nepal Academy of Science & Technology SPECIES RESPONSE TO CLIMATE CHANGE IN HIGH ALTITUDES initiative of a national organization in the Himalayan discourse _____________________________________________________ Nepal Academy of Science & Technology Advancing science and technology for all-round national development • Establishment 1982 • Autonomous & Statutory • Role envisaged: Think Tank Innovator Catalyst Facilitator The Initiation PYRAMID LABORATORY MOU between NAST & EvK2CNR in 1988 Pyramid Lab. built in 1990 Features: Glass & Aluminium, 3storied, Ht 8.4m, Alt. 5,050m asl The Activities PYRAMID LABORATORY Research Areas: i. Environment, ii. Biodiversity, iii. Earth Sc, iv. Medicine & Human Physiology, and v. Clean Technology Missions conducted >500 involving143 scientific institutions from several nations. NAST’s Initiatives RESEARCH IN HIGH ALTITUDES Anthropogenic Activities Biodiversity Knowledge Climate Change Impact Climate Change Studies MAJOR AREAS Baseline Inventories 1) Agrobiodiversity 2) Mushroom diversity 3) Herbaceous vegetation Dendro-climatological Studies 1) Reconstruction of env. history 2) Relationship between temp. & vegetation shift Baseline Inventories AGRO-BIODIVERSITY Study Area Namche, Khumjung, Phortse, Dole, Luza, Fanga, Machermo, Gokyo, Tengboche, Debuche, Pangboche, Dingboche, Pheriche, Jorsalle, Monju and Phakdin (16 settlements) Methodology Questionnaire survey, sample collection & analysis Baseline Inventories AGRO-BIODIVERSITY Major Findings Upper Limits (m asl) Staple crops: Barley 4,350; Buckwheat 3,930 Vegetables: Coriander 4,480, Radish/Turnip/Onion/Peas 4,359 Cauliflower, Carrot 3,930 Potatoes 4,700 (Tarnak) Ref. D Bhuju, A Giri, P Rana 2007 Baseline Inventories MUSHROOM BIODIVERSITY Study Area: SNP Methodology Field visit, Collection & analysis Major Findings Richness 150 spp. Used locally 29 spp. Highest 3,500-4,000m asl Ref. A Giri, P Rana 2006 Baseline Inventories HERBACEOUS DIVERSITY Study Area Imja Valley 3,400-4,650m asl Methodology Sampling, Collection, Analysis Major Findings Richness 180 spp, Location recorded, 32 spp in higher range than previously reported Ref. E Paudel, D Bhuju, K Shrestha 2007 Climatic Impact DENDRO-CLIMATOLOGICAL STUDY Objective Understand the impact of climate change on the distribution of forest vegetation in the Himalaya Methodology 1. Set-up permanent plots 2. Tree inventory 3. Tree core collection & analysis Site Tree-line Climatic Impact DENDROCHRONOLOGY Trees are nature’s ultimate environmental monitoring stations, make annual rings Dendrochronology, Method of scientific dating based on the analysis of tree-ring growth patterns Tree rings are called proxyclimate indicators Dendro-climatological Study PERMANENT PLOTS Pangboche, 4,050m asl Deboche, Alt. 3,850m Dendro-climatological Study RESULT: FOREST STRUCTURE BA (cm2/ha) SPECIES Panboche Debuche Panboche Debuche 79059.2 68228.8 120 359 27831.9 84990.3 204 149 4785.0 15030.5 117 279 111862.1 186107.6 445 1034 Abies spectabilis Betula utilis Sorbus microphylla TOTAL DENSITY (n/ha) ____________________________________________________ MEAN DBH SPECIES MAX DBH Panboche Debuche Panboche Debuche Abies spectabilis 24.9 8.5 68 99 Betula utilis 11.6 24.0 40 63 Sorbus microphylla 5.7 13.6 7.4 10.4 39 68 36 99 TOTAL Dendro-climatological Study TREE CORE COLLECTION Core Collection Abies spectabilis Juniperus recurva Betula utilis Total About 300 from various sites Preservation, Mounting & Sanding Dendro-climatological Study TREE CORE ANALYSIS Bell shaped, poor regeneration in recent years Inverse J, accelerating recruitments in recent years Average age: Panboche 64 yrs; Debuche 64 yrs Max. age: Panboche 147 yrs; Debuche 207 yrs Climatic Impact DENDRO-LAB Lab Facility: 1. Lin-Tab digital positioning table for tree-ring analysis 2. Leica S4E stereo microscope 3. LintabTm swing arm stand 4. TSAP-Win Prof. software Climatic Impact DENDRO-TRAINING WORKSHOP Date: 15-22 Jan 2008 Total Participants: 18 Resource Persons: Univ. of Padova Participating Institutions • Central Dept of Env Sc. Tribhuvan Univ. • Department of Plant Resources, GON • The Standard Nursery Pvt Ltd • Nepal Academy of Science & Technology • College for Applied Sciences • Dept. of Forest Research & Survey, GON • Dept of Hydrology & Meteorology, GON • National Trust for Nature Conservation • Dept. of National Parks & Wildlife Cons. • Ethnobotanical Society of Nepal • Madan Puraskar Guthi • Central Dept. of Botany, TU Climatic Impact DENDRO-CLIMATOLOGICAL STUDIES Langtang National Park NP Gaire, YB Dhakal, H Lekhak 2008; TU Abies spectabilis; Core: 210 Manaslu Conservation Area M Suwal 2009 UIB-TU; Gaire & Bhuju 2010 Abies spectabilis; Core: 148+ Manang (trans-Himalaya) KB Shrestha 2009; UIB, Norway Pinus roxburghii; Core: 133 Mustang (trans-Himalaya) E Udas; UG; Germany Abies spectabilis; Core: 109 Kathmandu Valley NP Gaire & DR Bhuju, NAST Pinus roxburghii; Core 65 Climatic Impact RESULTS: MANASLU There was new recruitments of seedlings and saplings in tree-line ecotone. The species limit has advanced from 3,673m asl in 1958 to 3,841m asl in 2007 with a total of 168 m upslope shift at the average rate of 34.29 m per decade. The seedlings below tree-line have comparatively faster growth. ______________________________ Ref. M. Suwal 2010 Climatic Impact RESULTS: MANASLU Abies spectabilis Transect 1 Transect 2 Betula utilis Transect 1 Transect 2 Species 3984 limit/line 3955 3996 4003 Tree line 3830 3996 4003 3907 Preliminary result: upward migration of Abies spectabilis by >1m/yr Ref. Gaire & Bhuju 2010 Climatic Impact RESULTS: LANGTANG 1. There was significant -ve correlation between the tree growth & mean monthly min. temp. of Mar & Apr of the current year, Oct of the previous year, and mean of Mar-May temp. of the current year. 2. Though statistically insignificant, there was +ve correlation between ring width and mean monthly precipitation of the most of the months of current year and -ve correlation with previous year’ precipitation. ________________ Ref. NP Gaire 2008 Climatic Impact RESULTS: MUSTANG The positive response of temperature (previous Nov, current Feb-Mar-May) during the early and mid 20th century was either both discontinuous and showed no correlation with tree growth at later period (Feb-Mar) or it turned to be negatively associated with growth (previous Nov and current May). This recent change in sensitivity of tree growth and temperature variability was unclear. ____________________ Ref. E Udas 2010 Climatic Impact WHAT NEXT Extend the study area Strengthen the Dendro-Lab International collaboration