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8/9/2019 Climate Change and Forest Insect-Pests
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TheGreeneryajournalofEnvironmentandBiodiversity7(1)September2009 Jha
ClimateChangeInducedPotentialImpacts(ecophysiological)onInsectPestsin
NepaleseForests:ASynopsisforFutureResearchandManagement
BidyaNathJha
Asst.Research
Officer,
Department
of
Forest
Research
and
Survey,
GPO
3339,
Kathmandu,
Nepal.
ResearchStudent,FacultyofLifeSciences,UniversityofCopenhagen,Denmark.
Email:[email protected];[email protected]
Abstract:
Thisstudyaimsatreviewingtheavailableliteraturesontheecophysiologicalimpactsofclimatechangeonforest
insectpests and its hosts. Methodology adopted for preparing the paper is the critical review of literatures
available inCopenhagenUniversitysLife librarydatabases.Withstandingwiththeglobalprojectionsofclimate
change, Nepal will experience a noticeable rise in temperature and changed rainfall pattern throughout the
country inyears to come.These changes can createmixedecophysiological impactsover the insectpestsof
NepaleseForests.Inthelightofstatisticsonprevailingclimate,projectedclimaticconditionsandforesttreesand
associated insectpests inNepal; the insectpests invasion seems to be obvious than before.Altered climatic
trends invite conditions like expansion of natural range by forest insectpests adapting to new environment.
Insectpestscanalsoswitchtheirhostbyturningthemselvespolyphagoustomeetthenutritionalrequirementin
new climatic conditions. Besides, advancing their physiological and phenological processes and reducing the
vulnerabilityofbeingpredatedareotherpotential impacts that canhappen to insectplant interaction in the
futureclimaticscenarios.Thesechangesinturnareexpectedtohinderthevitalforestryfunctionsthroughpest
damageincludingcarbondioxidesequestrationcapacityofforestsinNepal.
Key Words: Climate change, ecophysiological impacts, range extension, phenology, insectspests, diapause,
Nepal,morphogenesis
BACKGROUND:
Insectspests are one of the major ecological components of forest ecosystem but their contributions and
ecologicalroles inglobalchangeandforestryhaveoftenbeenoverlookedandneglected.Thecontributionand
ecologicalprocessesassociatedwithforestinsectpestsarebothpositiveandnegativefortheforestecosystem.
To illustrate, these groups contribute to the natural regeneration of plant through its remarkable role in
pollination.Ontheotherhand,theyarealsoresponsibleforcommercial lossthroughtissuedamageofwoody
componentofforestsandsignificantreductionofforestsnaturalcapacitytofixtheatmosphericcarbondioxide
inmultipleways.Manystudiesfromdifferentpartoftheworldsuggestthatinsubarctic,borealandtemperate
foreststheaverageconsumptionforminsectherbivoryrangesfrom110%offoliageofdominanttreespecies.In
specificcase
of
temperate
broadleaved
forests,
for
example,
an
average
of
7.1%
of
damage
is
reported
by
forest
insectpests(ColeyandBarone,1996).
History of extreme outbreaks of the insectpests in different forest types of the world in last century have
compelledthescientiststostudytheassociatedlinkbetweenclimatechangeandoutbreakeventsinthecourse
oftime.DuetosharpvariationsinaltitudefromSouthtoNorth,Nepaloffersluxuriousmicroclimaticgradientsto
differentgeneraandspeciesofforestinsectspestsinNepal. Thapa(1997)hasenumeratedapproximatelyover
fivethousandsofinsectspeciesfromNepal.Alargernumberofforestpestsarereportedtodamagebothnatural
and plantation forest of Nepal. Although numerous published and unpublished literatures exists about the
incidentaloutbreaksof forestpestepidemics inNepalandoutside in recentyears (Jackson,1987;FAO,2003;
Jakobet al., 2007; FAO, 2007; FAO, 2009), its link with climatic variables and statistics on the damage
assessmentsare lacking inNepal.Anothergroupofstudiesofrecentdecadesonplatpests interactions (Coley
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TheGreeneryajournalofEnvironmentandBiodiversity7(1)September2009 Jha
andBarone,1996;FAO,2007;FAO,2009)mostlyconcludethatdamagesofwoodyplantsbytheseorganismsare
goingtoincreasewithalteredtemperatureandprecipitationregimesinyearstocome.
Therefore,thisstudyaimsatevaluating theavailablestudieson theclimatechange impactson forest insects
pestsecophysiology.Theintentionistoelaboratearesearchandmanagementdimensioninplantandinsects
pests interactionwhichNepalese forestsmay face indifferentclimaticpredictionsforthe future.Thispaper is
basedontheassumptionsthatscientificstudyofclimatechangeimpactsoverforestinsectpestsecophysiology
ontheotherpartoftheglobecanalsobegeneralizedinNepaleseconditionswithsomecasespecificexceptions.
Nonetheless,majorityof review isbasedon thestudiesconducted insimilarconditions throughout theworld
ratherthanbeingconfinedtoNepaleseforests.Oneofthemanybasesforadoptingthisapproachforthestudyis
therevelationthatNepalsclimatictrendsarenotsurprisinglydissimilartorestoftheworldespeciallyNorthern
Hemisphere(Shresthaetal.,1999).METHODOLOGY:
This review is based on the desk study of different literatures from secondary, published and unpublished
sourcesavailable
either
in
print
or
digital
media
into
the
LIFE
library
databases
of
Copenhagen
University,
Denmark.The firststepwas toestablishdifferentsearchparameters forthe literaturehuntwithcoinedstudy
objectivesforthewriting.ThesearchparametersortermswereexclusivelyappliedintothedifferentLIFElibrary
database system for finding out the available resources (Annex 1). Out of the massive hits found, selected
number of relevant literatures especially international journal articles, books and research papers were
scrutinizedandrankedforthereviewpurpose.Objectiveorientedclassificationofliteratureswasperformedand
ultimate reviewsourceswereachieved.Priority for thereviewwasgiven for thosearticlesor researchpapers
whichwereappearingrelativelyrecent,studiedfromtheprimarysourcesofinformationandthestudyareawas
Nepal or the vicinity or from similar conditions. Consultations from the lecturers (2), library staffs (3) and
graduatescholars(2PhD;and5M.Sc.)wereothersourcesofinformationforfurtherliteratureandinformation
forthereview.
RESULTANDDISCUSSION:
PastandprojectedclimateTrendsinNepal:
An intensiveanalysisofmaximumnumberofmeteorologicaldataofyearsbetween1971and1994 (collected
from49numbersofmeteorologicalstationsfrommidhillsandmountainsand14numberofstationsfromTerai
andSiwaliks)revealsthatthemuchdiscussedclimatechange(especiallyincreaseintemperature)istakingplace
inmorethananticipatedrateinthecaseofNepal(Shresthaetal.,1999).Therateoftemperatureincreaseperyearwerefoundtobe0.06
0Cto0.12
0Cincaseofmidhillsandmountainand0.03
0Cforthecaseoflowland
Nepal (Shresthaetal.,1999).The temperaturedifferencesarehigherandpronounced in thedrywinter spellthan the monsoon and pre monsoon records. Before the year 1978, temperatures of the five development
regions,nationalaverageand individualstationsweremostlyconstantordecreasing,however,after1978 the
generaltrend
for
all
regional,
national
and
stations
temperature
were
found
increasing.
This
study
also
found
thattheseasonalandspatialdistributionofwarmingtrends inNepalhasalsoaconsiderablebearinguponthe
monsooncirculationofthecountry (Shresthaetal.,1999;Shresthaetal.,2000).Moreover,therelatively longtemperature recordsofKathmanduValley (since1921)demonstrated the samepatternofwarming trendsas
observed in Northern Hemisphere by different studies, which in turn indicates that there exists relationship
betweenglobalclimatechangetoNepalswarmingtrend(Shresthaetal.,1999).TemperaturetrendanalysisforSouth Asia (IPCC, 2007), which also bears an indirect implication for Nepals temperature trend, has been
reproducedinFigure2.
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Table 1: Temperature Trend of Nepal (Positive Numbers for Increasing trend and negative numbers for
decreasingtrends)
MeanTemperatureTrendinNepalbyRegions19771994(0C)(Shrestaetal.,1999)
Winter (Dec
Feb)
Pre Monsoon
(MarMay)
Monsoon (Jun
Sep)
Post Monsoon
(OctNov)
Annual
(JanDec)
TransHimalayas 0.124 0.005 0.109 0.099 0.09
Himalayas 0.09 0.05 0.062 0.075 0.057
MiddleMountain 0.059 0.05 0.055 0.094 0.75
Siwalik 0.015 0.01 0.021 0.077 0.041
Terai 0.006 0.004 0.014 0.069 0.041
Nepal 0.061 0.032 0.051 0.081 0.059
Temperaturevariationsintable1havealsobeensupportedbyotherstudiesinNepalandinthevicinity.Sanoetal. (2005), for instance,has found thatwinter temperaturehasbeen significantly increasing inwesternNepal
since last400yearsbasedonhisdendrochronologicalanalysisofAbiesspectabilis tree rings.SimilarlyLiuandChen(2000)alsofortifiedtheabovetrendswiththeirrespectivestudiesintotheTibetanPlateau(othersideof
Himalayas)fromtheanalysisofclimaticrecordsofmorethanfourdecades.
Figure1:TemperatureTrend(AnnualMeanMaximum)inNepal(Shresthaetal1999,inWWF,2005)
Basedonthehistoricalchanges inglobalclimate, IntergovernmentalPanelonClimateChange(IPCC)hasmade
scientificpredictions
for
the
climatic
anomalies
under
different
emission
(Low
and
High)
conditions
and
time
horizons(baseyearslongterm:2080;mediumterm:2050andshortterm:2020)forglobalgeographicalareason
theearth (IPCC,2007).Although IPCC report (IPCC,2007)havenot includedclimaticpredictionexclusivelyon
Nepal,butpredictionsforthecountryhasbeenmade intothebroaderframeworkofSouthAsianregion.Also,
this report includes thevulnerabilityanalysisonSouthAsian level for theclimatechange impactondifferent
areas.Biodiversityhasbeenidentifiedasoneofthemostvulnerablesectorwith 2vulnerabilityscoreandwith
veryhighconfidencelevelforpredictiontobeimpactedbythesepredictedclimaticanomalies.
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Table2:PredictedvariationinprecipitationforSouthAsea
PredictedChangeinPrecipitation(%)forSouthAsia(IPCC,2007)
ShortTerm(2020) MediumTerm(2050) LongTerm(2080)
Periodof
the
yearLow
EmmissionHigh
EmmissionLow
EmmissionHigh
EmmissionLow
EmmissionHigh
Emmission
December
February
4 3 0 0 6 16
MarchMay 8 7 24 26 20 31
JuneAugust 7 5 11 13 15 26
September
November
3 1 6 8 10 26
Figure2:PredictedVariationinTemperatureforSouthAsia
In addition to IPCC projection, Nepal specific predictions have also been made recently through adopting a
number of climate prediction models (Agrawala et al., 2003). The brief, the result for the projection oftemperatureandprecipitationshavebeenreproducedintable3:
Table3:PredictedvariationsinTemperatureandPrecipitationinNepal
PredictedChangeinClimaticVariablesforNepal(Agrawalaetal.,2003)Temperature(
0C) Precipitation(%)
Year Annual DecFeb JunAug Annual DecFeb JunAug
2030 1.2 1.3 1.1 5 0.8 9.1
2050 1.7 1.8 1.6 7.3 1.2 13.1
2100 3.2 3.2 2.9 12.6 2.1 22.9
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ClimateChangeImpactsonForestInsectPests
Aswiththeotherbiologicalorganism,the lifecycleof forest insectpestsarehighlydependentontheclimatic
conditions of a particular locality, with well defined threshold levels of survival or maximal growth and
development.Numerousstudies (Beeson,1941;Nair,2007;Evans,2008)describethecriticalclimaticvariables
which
have
deterministic
role
in
the
survival
and
growth
of
forest
insect
pests
with
respect
to
its
stages
of
life
cycle.Inbrief,mostofthestudiessofarconducted,haveagreedthattheexpectedclimaticchangesaregoingto
promotethe lifecycle,growthanddevelopmentofthemajorityof forest insect pests ingeneral.Withspecial
referencetoNepalconditions,followingaresomeofthemostvisiblepotentialimpactsthatclimatechangemay
causeontheforestinsectpestsandtherespectivehosts(Nair,2007;Evans,2008):
RangeextensionofForestInsectsPests:
The most pronounced impact of increased temperature over the insectpests is their migration towards the
northernforesthabitats.Althoughclimatechangeimpactsonforestinsectsandtheirmigrationpatternhasnot
been studied inNepal, therearenumberof internationalexampleswhich canbeused to simulate the forest
conditionsinNepal.Forinstance,asurveyconductedbyPermesanandYohe(2003)ontheinsectreciprocation
ofclimatechangeconcludedthatamongthesurveyedspecies80%ofthesurveyedspeciessiftedtheirnatural
rangetowardsthenorth withanaveragerateof6kmin10years.Similarly,Evans(2008)presentedthespecific
caseofPineprocessionarymoths(Thaumetopoeapityocampa)northwardjourneyfromperipheryofOrleanstoasnorthasFontainbleau inFrance. Itshifted itsnaturalrangeofoccurrenceby87kmsince1972to2004,with
acceleratedrateoftravelinlasttenyears(56km).Usingthehistoricaldataof100years,Jepsenetal.(2008)haverecentlydocumentedhowtwospeciesofforestinsect pests,viz.OperophterabrumataandEpirritaautumnatashifted their range in last two decades in subarctic birch forest of Norway. These studies coincide on a
conclusionthatthechangesinglobalclimatehavepromotedforestinsect peststoexpandtheirrangetowards
thedirectionofthehigheraltitudesandlatitudes.ImportanceoftheknowledgefromthesestudiesinNorthern
HemispherecouldberelatedtoNepalesecontextsbecauseofNepalssimilarity inclimaticchangetrendswith
NorthernHemisphere(Shresthaetal.,1999).RangeJumpandAccommodation:
Rangejumpisanothersortofphenomenonassociatedwithforestinsectpestsintheadventofclimatechange.
Forest/plantproducttradesareoneofthemaincausesamongothersthatcarrythehighriskofrangejumpor
accommodation of non native species into the Nepalese forest areas.There are numerousexamples where
seeds are imported for the plantation activities in Nepal e.g. Eucaplytus specie and Leucaena species from
Australia,CryptomeriaspeciesfromJapanandmanymorefromIndiaincludingTectonagrandis,DalbergiaSissooandAcaciacatechu(Jackson,1987).Innewclimaticconditionsinthefuture,therewillbenowonderiftheAsianlonghornbeetle(Anoplophoraglabripennis),(manybroadleavedbased)whichisnativetotheregionsofJapan,ChinaandKoreaandhasalreadyfoundinUSandCanadathroughtrade(Bond,2008;FAO,2009),orothersimilar
destructive pests, will be brought to Nepal through plant product transactions (especially seeds) from other
regionorcountries.
ImpactonInsectsPestsPhenology:
Climatechangeconditionsmay impact toadvance someof thephenologicaland lifecycleprocesses in forest
insectpests. Permesan and Yohe (2003) found in their study that about 87% of inventoried insect species
showedadvancementincertainphonologicalprocesseslikefloweringorspringmigrationduetothepastchange
in the climate. Number of eggsper generation laid byHoplocerambyx spinicornis (a serious threat to Shorearobustatrees inNepal) ranges100300andviabilityof theeggsrangesbetween75%and100%dependingon
temperature and moisture conditions (Beeson, 1941; Nair, 2007). Warming induced conditions can create
favourablemicroclimaticconditionstorealizethisdestructivepestshigherrangeofviability(i.e.100%)inNepal.
Besides,thelarvalphasewhichisresponsibleformaindamageinthewoodandremainsfor610monthscanbe
prolongediftemperatureconditionsarefavoursinthefuture.
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Climatechangeisalsogoingtoimpacttherelationshipofforestpestswithitsnaturalenemiesthroughreducing
the riskystagesofbeingpredated,e.g. larvaandpupation, throughtheenhancedspeedof lifecycle.Relative
warming in winter (as predicted) advances the early stages (winter dormancy; eggs and transition between
dormancyandactivestage)andthereforereducesthechancesofbeingpredated(Bernays,1997;Evans,2008).
Developing
host
generality
over
the
host
specificity
in
Forest
Pests:
ThereareanumberofforestinsectsinNepalwhichshowsthecharacteristicsfeatureofdependingononlyone
host tree species e.g. Hoplocerambyx spinicornis (Sal Borer). However, due to reduced nutritional value(especiallyNitrogencompounds)oftree leaves inresponsetoelevatedtemperatureandcarbondioxide inthe
atmosphere, the probability of a specific pest to switching its host, i.e. turning from monophagous to
polyphagous,becomeshigher(Battisti,2008;Huntetal.,2006)ImpactsonInsectsPestsPhysiology:
Globalwarmingcan impact the reproductive, survival,growthanddevelopmentpotentialof forestpests.The
riseof temperaturemaysignificantlyenhance the reproductivecapacity in forestpestsbyadvancing their life
cycleactivitiesandshorteningthegapbetweeneachstage.YamamuraandKiritani(1998)mentionsthatariseof
20Ctemperature
(which
is
predicted
for
Nepal
for
next
50
years)
may
give
rise
of
one
to
five
additional
pest
generationsperyear,andincaseofdifferentspeciesofaphids,theratebecomeshigher.Anumberofforesttree
specieshavealreadybeenreportedtobedamagedbydifferentspeciesofaphidsinNepale.g.Alnusnepalensis,PiceasmithianaandAcerOblongum(Jackson,1987).Wintermortality in insectpests iscommonphenomenabecauseof the low temperature.Reduction inwinter
cold is removing the major control factor of insectpests in altitudinal and latitudinal temperate region
(Harringtonetal.,2008).Manyhighaltitude(above2000m)forestpestsbasedonWillow,Birch,Ash,Spruceandotherhighaltitude coniferousandbroadleaved speciesofHimalayas shows this remarkabledormancyperiod
betweenDecembertoMidMarch(Beeson,1941;Nair,2007).Impactofincreasedwintertemperatureongreen
spruceaphid(Elatobiumabietinum)populationhavebeenstudiedwithmostrecentdatasetof41yearsinSouthEngland(WestgarthSmithetal.,2007).Thisstudyfoundthatifthewintertemperatureisgoingtoincreaseby230C,whichalso is thepredicted rise in temperature fornext50100years inNepal (Shresthaetal,1999), the
aphidmayrealizeitsbioticpotentialofreproductionandcausespruceepidemicsinthatareainyearstocome.
TheForestResearch(2008)ofUKForestryCommissionpointoutthatincaseofanoutbreakofspruceaphid,the
growthofinvadedtreemayreduceupto30%inayear,andincaseofrealizedbioticpotential,thedamagemay
yieldmorethanbeingexpected.
Manyofinsectspests,especiallyfrommiddletohigheraltitudesandlatitudes,haveapronouncedcharacteristic
of suspending their metabolic activities temporarily during their life cycles due to a process being known as
diapause. The stage is further characterized by decreased level of morphogenesis, increased level of
environmentalresistance,andreducedconsumptionofplantmaterialbythepests(Tauberetal.,1986).Climate
change (raisedtemperature)mayactasexternalenvironmentalstimulation forbreaking thediapausestage in
forestinsectpestsinadvanceandactivatetheirphysiologicalprocessessothatmoreconsumptionofplanttissue
becomesobvious(Battisti,2008).
ImpactsonHosts
Theavailabilityofextralevelofatmosphericcarbondioxideduetoclimatechangeenhancesthefoliargrowthin
trees which further imbalances the natural carbon nitrogen (C/N) ratio. An experimentation on Impact of
endemicinsectherbivoryonstructureandproductivityofvegetationinNorthernEuropefoundthatplantgrown
inelevatedcarbondioxide(CO2)concentrationhavelowernitrogenconcentrationsandhigherconcentrationof
non structuralcarbohydrates (Kozlov,2009).Thischange inducednitrogendeficiencyand imbalances inother
nutritional value of the forest vegetation become insufficient to meet the metabolic requirement of
phytophagous insects (pests)qualitatively.This in turn forced them toconsumemorequantitiesofvegetative
materialsto fulfiltheirnutritionaldemand tocompensatereduced foodquality (AyresandLombardero,2000;
Kozlov,2009;
Battisti,
2008;).
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Theclimatechangeinduceddroughtisreportedtodevelopakindofstressgradient,anddeclineinthestomatal
conductance of the forest trees which make them more prone to the insectpests attack (Scarr, 1998). Sal
(Shorearobusta)trees,forexample,havebeenfoundtobemoreattackedonthenutrient(includingwater)poorsitese.g.ridgesandsandysoilsthanonambientconditionsbySalborer (Hoplocerambyxspinicornis) (Jackson,1987;Nair,2007).Intheconditionofsummerdrought,whichisapredictedconditioninNepal;manyIpsspecies(64worldwide) (FAO,2009), the pine bark beetles, are expected to invade the coniferous plantations in thesubtropical to lowertemperateregionsofNepal.KhoteSalla (Pinus roxburghii) forestarehighlysusceptibletoincreased damage by this kind of beetle mostly because it has most of its area under high prone zone for
summerdroughtaspredictedbyabovementionedsourcesinNepal.
CONCLUSION:
ClimatechangeisoccurringinanalarmingrateandatanextentthatresearchersusedtoanticipateforNepal.It
hasvarietyofdirectandindirectbearingsovertheabioticandbioticsystemsofNepal.Higherclimaticvariations
andtheresultantforesttypesofNepalofferhomeforavastnumberofforestinsectpests.Thesetinycreatures
have often not been given due attention by the researches despite the fact that damages caused by these
organismsaresignificantand increasing.Forestbased insectpestsand itsextent,magnitudeand frequencyof
damagesand
its
relation
with
climatic
variations
need
to
be
assessed
scientifically
before
any
serious
damage
is
causedinforestsofNepal.PredictionfortemperatureriseandalteredprecipitationpatterninNepalshouldbe
taken as one of the potential threats for the commercial objectives of forestry in Nepal. Host changing and
realizationofbioticpotentialbydestructiveforestpestsmaygiverisetoseriouseconomicandecologicalthreat
inmultiplewaysinNepaleseforestry.
ACKNOWLEDGEMENTS
MyspecialthanksgototheProfessorNielsStrangeforencouragingmeforthiswriting.Thesupportivehandsof
LIFElibrarystaffsforsearchingandavailingtherequiredarticlesinprintarealsohighlyacknowledged. Iamalso
humblythankfultoSHEACTeamandthepresident forprovidingmetheopportunitytopublish inthereputed
Greenery.
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Appendix1:Thesummaryofdatabasesearchrecordsfordifferentsearchparameters
Database/Search
Location
Searchterms/parameters Resulting
numbers of
references
Number of useful
references
CABABSTRACTS 1. Climatechange*2. ForestInsectPests*3. GlobalWarming*4. Joint search with 1,2 and 3 (using AND
operator)
5. Joint search with 1 , 2 and 3 (using ORoperator)
6. Carbon*Insects*Forests*7. ForestEntomologyand/orClimateChange8. EcophysiologyofInsects
1123
1527
2321
2576
2765
1656
1934
22
17
11
12
9
7(overlaps)
2
1
2
AGRICOLA
1. Climatechange*2. ForestInsectPests*3. GlobalWarming*4. Joint search with 1,2 and 3 (using AND
operator)
5. Joint search with 1 , 2 and 3 (using ORoperator)
6. Carbon*Insects*Forests*7. ForestEntomologyand/orClimateChange8. EcophysiologyofInsects
3467
946
2226
472
498
23
44
4
17(overlaps)
3
0
1
3
2
5
0
CAB ABSTRACT
ARCHIVE
1. Climatechangeforestpests* 45 7(overlaps)AGRIS
1. ImpactsofClimateChangeonInsects*2. ForestInsectsandClimateChange*3. Baseageinvariantmethod*
392
536
6
9
9
4
Google Search
(English)
1. ClimateChangeImpactsonForestPests2. NepalForestInsectsandClimateChange3. IndiaClimateChangeandForestInsects4. WorldClimatechangeandForestPests
860,000
10,400
35,000
67,700
18(10pagesonly)
6(10pagesonly)
11(10pagesonly)
4(10pagesonly)
GOOGLESCHOLAR 1. Climate Change in Nepal and Forest*Insects
2. ClimateChangeinIndiaandForest*Insects4,830
26,900
14(overlapping)
3(10pagesonly)
Personal Contact
(Lecturers/Library
staffs/fellow graduate
students)
1. Subjectiveconversation Altogetherthey
referredto9
number of
references
4(3overlapping)
Note:Thisisnotexhaustivelistofsearchhistorythattheauthorhasperformedforliteraturesearch.