Como las corrientes marinas, los sistemas montañosos y la linea ecuatorial al clima del continente americano?

Rcvdcvit {bc ivrct ts rcvvargvag tc sfadin cn ch `coatjcvag ngvrc q SNI rcvdcvi {cn ivrc ch` tsv coatjcvag.

Cn tcnrabg CITCh / tc gctrc cpracnbc bctbc HGT 43 »` ITRI HGT 9 = 4 »bc hgnmarsbgctrc.

Ch dgnrancnrc tc sfadi {{gv dgo hcrg cn ch `coatjcvag gddabcnrih.

Ch dgnrancnrc OET dcvding i Ioávadi ctItai ih gctrc BCH YSC Ioávadi ctre tc {{ivibi gvch Ctrvcd`g bc bc Fcvanm sngt 1 ; Lo ind`g aC.

CITCh tc {IVI hi {} Tc cnïntshi IVB (IhitliCtribgt Snabgt hi {bc bc cnïntshi D`slgrli (Vstai .

@idai ch ch ctrc dgnrancnrc OETdcvding i Ioávadi ct Éjvadi YSC batri sngt 4 oah lo bc nsctrvg dgnrancnrc i hi ihrsvi bcFvitah.

Ch dgnrancnrc iocvading haoari ih ngvrc DGN ch gdáing Mhidaih Évradg ih CITCh DGN chgdáing Irhénradg q ih gctrc DGN ch gdáing [idïjadg.

Ch hïoarc tsv dgvvct {i hi gnbc snaônBCH [idïjadg DGN ch Irhénradg .

Ctrit oitit bc IMSI hg {tc Ivin bc HGT grvgt dgnrancnrct.

Hgt {snrgt cprvcogt BCH rcvvargvag iocvading TGN HGT tamsacnrct5% Dgnrancnrihct.

Ih ngvrc [IRSN Fivvg}  cn Ihitli DGN = 9 »64 aC hirarsb ngvrc.

Ih tsvdifg jvg} ivb cn D`ahc DGN 32 »bc hirarsb TSV.

Ih ctrc difg Fvindg cn Fvitah DGN 42 - 2 = - bc hgnmarsb gctrc.

Ih gctrc difg [VINDA {c bc Mihct cn Ihitli Ctribgt Snabgt bcIoávadi DGN 9 : 1 »bc hgnmarsb gctrc.

Antshivct%.

Ih ngvrc difg Ogvvat Ects {cn  Mvgcnhinbai DGN 04 »bc hirarsb ngvrc.

Ihtsv golpeado Athit Bacmg Vioïvcu bc D`ahc DGN 3 : »4 ; - bc hirarsb TSV.

Ih ctrc golpeado AthitJcvninbg bc Ngvgùi CN - Fvitah DGN 46 »bc gctrc hgnmarsb.

Ih gctrc hi athi IRRO(Ihcsrainit Ctribgt Snabgt!

 DGN 9 = 4 »gctrc bc hgnmarsb.

6Hit BGT IoávaditHgt {bc iïtct Ioávadi TGN OSQ bajcvcnrct cnrvc tï ng tghg {ts gv nõocvg bc `ifarinrct g{GV CH rioiùg bc TST rcvvargvagt tang riofaán {ts gv` atrgvai cn grvit {{ihifvit gv ch{i vgdctg YSC hhczô ts jgvoidaôn.