...1680 SItlistname Stlistid1019352644SItlisttlisttemplateid-167586036
6tlistsimpleItlistleveltlevelnfc1tlevelnfcn1tlevelj
c0tleveljcn0tlevelfollo0tlevelstartat1tlevelspace0t
levelindent0Itleveltextt02t00.SItlevelnumberst01Stf
bias0 tfi-720tli840tjclisttabttx840tlin840 SItlistname Stlistid1081488372SItlisttlisttemplateid67698689tl
istsimpleItlistleveltlevelnfc23tlevelnfcn23tleveljc
0tleveljcn0tlevelfollo0tlevelstartat1tlevelspace0tl
evelindent0Itleveltextt01tu-3913 SItlevelnumbersStf3tfbias0 tfi-360tli360tjclisttabttx360tlin360 SItlistname Stlistid1709842253SItlisttlisttemplateid67698689tl
istsimpleItlistleveltlevelnfc23tlevelnfcn23tleveljc
0tleveljcn0tlevelfollo0tlevelstartat1tlevelspace0tl
evelindent0Itleveltextt01tu-3913 SItlevelnumbersStf3tfbias0 tfi-360tli360tjclisttabttx360tlin360 SItlistname Stlistid1912233134SSIttlistoverridetableItlistover
ridetlistid345904828tlistoverridecount0tls1SItlisto
verridetlistid1709842253tlistoverridecount0tls2SItl
istoverridetlistid1912233134tlistoverridecount0tls3
SItlistoverridetlistid1081488372tlistoverridecount0
tls4SItlistoverridetlistid1019352644tlistoverrideco
unt0tls5SItlistoverridetlistid906919080tlistoverrid
ecount0tls6SItlistoverridetlistid610010792tlistover
ridecount0tls7SSIttrsidtbl trsid15545977SIttgenerator Microsoft ord 10.0.2627SItinfoIttitle Ciclonii tropicaliSItauthor saSItoperator danielSItcreatimtyr2002tmo2tdy9thr13tmin32SItrevti
mtyr2002tmo2tdy9thr13tmin32SItversion2SItedmins3SIt
nofpages2SItnofords1035SItnofchars5906SIttcompany SItnofcharss6928SItvern16437SStmargl630 tidoctrltftnbjtaenddoctnoxlattoyentexpshrtntnoultr
lspctdntblnsbdbtnospaceforultformshadethorzdoctdghs
pace180tdgvspace180tdghorigin1701tdgvorigin1984tdgh
sho0tdgvsho0tjexpandtviekind1tviescale100tpgbrdrhea
dtpgbrdrfootthtmautsptnolnhtadjtbltrsidroot15545977 tfet0tsectd tlinex0tendnheretsectdefaultcltsftnbj Ittpnseclvl1tpnucrmtpnstart1tpnindent720tpnhang Itpntxta .SSIttpnseclvl2tpnucltrtpnstart1tpnindent720tpnhan
g Itpntxta .SSIttpnseclvl3tpndectpnstart1tpnindent720tpnhang Itpntxta .SSIttpnseclvl4tpnlcltrtpnstart1tpnindent720tpnhan
g Itpntxta SSIttpnseclvl5tpndectpnstart1tpnindent720tpnhang Itpntxtb SItpntxta SSIttpnseclvl6tpnlcltrtpnstart1tpnindent720tpnhang Itpntxtb SItpntxta SSIttpnseclvl7tpnlcrmtpnstart1tpnindent720tpnhang Itpntxtb SItpntxta SSIttpnseclvl8tpnlcltrtpnstart1tpnindent720tpnhang Itpntxtb SItpntxta SSIttpnseclvl9tpnlcrmtpnstart1tpnindent720tpnhang Itpntxtb SItpntxta SStpardtplain tqc tli0tri-270tidctlparttx900taspalphataspnumtfaautot
adjustrighttrin-270tlin0titap0tpararsid15545977 tfs20tlang1033tlangfe1033tcgridtlangnp1033tlangfen
p1033 Itfs36tcf1tinsrsid15545977tcharrsid15545977 Ciclonii tropicalitpar Stpard tqj tli1170tri-270tidctlparttx900taspalphataspnumtfaau
totadjustrighttrin-270tlin1170titap0tpararsid155459
77 Itf36tfs36tcf15tinsrsid15545977 tpar Stpardtplain ts15tqj tli720tri-270tidctlparttx900taspalphataspnumtfaaut
otadjustrighttrin-270tlin720titap0tpararsid15545977 tfs24tlang1033tlangfe1033tcgridtlangnp1033tlangfen
p1033 Itinsrsid15545977 SItinsrsid15545977 ttab SItinsrsid15545977 Sunt cicloni tropicali ai regiunilor intertropicale,adica depresiuni barice tropicale in care deplasarea aerului aflat in miscare depaseste 17ms sau 61 kmh. Daca viteza vantului depaseste 32 ms sau 115 kmh, se spune ca este vorba de un uragan.tpar Stpardtplain tqj tli720tri-270tidctlparttx900taspalphataspnumtfaaut
otadjustrighttrin-270tlin720titap0tpararsid15545977 tfs20tlang1033tlangfe1033tcgridtlangnp1033tlangfen
p1033 Itfs24tinsrsid15545977 SItfs24tinsrsid15545977 ttab SItfs24tinsrsid15545977 Cea mai mare parte a autorilor si publicatiilor, care se ocupa de problema catastrofelor naturale ce afecteaza omenirea, este de acord ca ciclonii tropicali pot provoca mai multi morti si mai multe distrugeri decat aproape oroce alta dintre numeroasele forte ale naturii. Tocmai de aceea cercatarilor privitoare la geneza si evolutia ciclonilor tropicali li se acorda o atentie deosebita in numeroase tari, cu precadere in cele afectate de aceste fenomene extrem de violente si daunatoare. tpar Stpard tqj tli0tri-270tidctlparttx900taspalphataspnumtfaautot
adjustrighttrin-270tlin0titap0tpararsid15545977 Itfs24tinsrsid15545977 SItfs24tinsrsid15545977 ttab SItfs24tinsrsid15545977 Pentru formarea ciclonilor tropicali sunt necesare cinci conditii si anumetpar Itpntexttpardtplaintf3 tlochtaf3tdbchtaf0thichtf3 tb7ttabSStpard tqj tfi-360tli1080tri-270tidctlparttx900Ittpn tpnlvlblttilvl0tls3tpnrnot0tpnf3tpnstart1tpnindent
360tpnsp120tpnhang Itpntxtb tb7SStaspalphataspnumtfaautotls3tadjustrighttrin-2
70tlin1080titap0tpararsid15545977 Itfs24tinsrsid15545977 suprafete oceanice vaste, cu temperaturi ridicate 26.5 SItfs24tinsrsid15545977 ItfieldIttfldinst SYMBOL 176 ttf Symbol tts 12SItfldrslttf3tfs24SSSItfs24tinsrsid15545977 C deasupra carora aerul este cald si umedtpar Itpntexttpardtplaintf3 tlochtaf3tdbchtaf0thichtf3 tb7ttabSStpard tqj tfi-360tli1080tri-270tidctlparttx900Ittpn tpnlvlblttilvl0tls3tpnrnot0tpnf3tpnstart1tpnindent
360tpnsp120tpnhang Itpntxtb tb7SStaspalphataspnumtfaautotls3tadjustrighttrin-2
70tlin1080titap0tpararsid15545977 Itfs24tinsrsid15545977 valori suficient de mari ale fortei Coriolis, pentru a determina miscarea turbionara a aeruluitpar Itpntexttpardtplaintf3 tlochtaf3tdbchtaf0thichtf3 tb7ttabSStpard tqj tfi-360tli1080tri-270tidctlparttx900Ittpn tpnlvlblttilvl0tls3tpnrnot0tpnf3tpnstart1tpnindent
360tpnsp120tpnhang Itpntxtb tb7SStaspalphataspnumtfaautotls3tadjustrighttrin-2
70tlin1080titap0tpararsid15545977 Itfs24tinsrsid15545977 lipsa unei componente verticale slabe in centrul de bazatpar Itpntexttpardtplaintf3 tlochtaf3tdbchtaf0thichtf3 tb7ttabSStpard tqj tfi-360tli1080tri-270tidctlparttx900Ittpn tpnlvlblttilvl0tls3tpnrnot0tpnf3tpnstart1tpnindent
360tpnsp120tpnhang Itpntxtb tb7SStaspalphataspnumtfaautotls3tadjustrighttrin-2
70tlin1080titap0tpararsid15545977 Itfs24tinsrsid15545977 preexistenta unei perturbatii tropicale ce actioneaza ca sursa a viitorului ciclontpar Itpntexttpardtplaintf3 tlochtaf3tdbchtaf0thichtf3 tb7ttabSStpard tqj tfi-360tli1080tri-270tidctlparttx900Ittpn tpnlvlblttilvl0tls3tpnrnot0tpnf3tpnstart1tpnindent
360tpnsp120tpnhang Itpntxtb tb7SStaspalphataspnumtfaautotls3tadjustrighttrin-2
70tlin1080titap0tpararsid15545977 Itfs24tinsrsid15545977 scurgerea aerului pe suprafata perturbatiei.tpar Stpard tqj tli720tri-270tidctlparttx900taspalphataspnumtfaaut
otadjustrighttrin-270tlin720titap0tpararsid15545977 Itfs24tinsrsid15545977 SItfs24tinsrsid15545977 ttab SItfs24tinsrsid15545977 Energia necesara formarii si dezvoltarii ciclonilor in general, se datoreaza neomagenitatii temperaturii maselor de aer care genereaza gradientii barici orizontali. In cazut ciclonilor tropicali, sursa principala de energie cinetica o constituie insa instabilitatea verticala deosebit de mare la latitudinile respective. Totodata, sursa de energie necesara mentinerii acestor cicloni este caldura latenta de evaporare,eliberata prin condensarea...
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