Download full issue - PanamJAS

More documents

Recommendations

Info

200J. L. NICOLODI & R. M. PETERMANNFigure 15. Vulnerability of the northern part of the South Region. The topography, population density, and socioeconomicfactors of urban centers generate medium to high vulnerability levels.Figure 16. The high and very high vulnerability region corresponds to the distal portion of the Itajaí-Açu River basin,which has undergone frequent inundation in recent years, particularly during recent events in 1983, 1984, and 2008.Pan-American Journal of Aquatic Sciences (2010), 5(2): 184-204
Potential vulnerability of the Brazilian coastal zone201million people were injured, <strong>full</strong>y confirmed thisvulnerability (Fig. 16).The southern part of Santa Catarina state upto the border of Uruguay, is characterized by sandybarriers highly exposed to a strong wave and stormregimen with a tidal range of less than 1 m.Numerous lagoons developed behind the barrierswith only few outlets.Although the geomorphological contextalone cannot explain the high vulnerability levels, itis important to emphasize that this region is criticalfor the occurrence of uncommon, extreme events ofgreat magnitude, as was the case of CatarinaHurricane, which struck in 2004 and all but wipedout the bordering area between the two southernmoststates of Brazil.The only place defined as highly vulnerablein Rio Grande do Sul state is the Rio Grande areanear the Patos Lagoon outlet, which is kept openthrough two 4.5 km long jetties (Rio Grande barpiers). This scenario includes the main urban centerin the inner estuary, with a population of around200.000 inhabitants living on low, flat ground andover areas expanded by the water surface landfill.The land occupied by housing coexists with spacesdominated by the activities of one of the country’smost important ports, combined with an expandingmanufacturing and petrochemicals complex of greatrelevance to the state (Fig. 17).The role of the port of Rio Grande in thispart of the area of high vulnerability, should be consideredin conjunction with the Metropolitan AreaFigure 17. From the south of Santa Catarina state to the border of Uruguay, vulnerability is relatively low, with theexception of the urban area of Rio Grande. This region is subject to weather events of great magnitude, such asHurricane Catarina in 2004.Pan-American Journal of Aquatic Sciences (2010), 5(2): 184-204
Page 3 and 4: PAN-AMERICAN JOURNAL OF AQUATIC SCI
Page 5 and 6: Representations in the Brazilian me
Page 7 and 8: IIM. S. COPERTINO ET ALLIIntroducti
Page 9 and 10: IVM. S. COPERTINO ET ALLIpollution
Page 11 and 12: VIM. S. COPERTINO ET ALLIpublic pol
Page 13 and 14: VIIIM. S. COPERTINO ET ALLINicholls
Page 15 and 16: XC.A.E. GARCIA & C.A. NOBREimplemen
Page 17 and 18: Brazilian coastal vulnerability to
Page 29 and 30: Potential vulnerability of the Braz
Page 36 and 37: 192J. L. NICOLODI & R. M. PETERMANN
Page 50 and 51: 206L. F. D. FARACO ET ALLIIntroduct
Page 52 and 53: 208L. F. D. FARACO ET ALLIclimate c
Page 54 and 55: 210L. F. D. FARACO ET ALLIfocused o
Page 56 and 57: 212L. F. D. FARACO ET ALLIIn spite
Page 58 and 59: 214L. F. D. FARACO ET ALLIand ecolo
Page 60 and 61: 216L. F. D. FARACO ET ALLIconsideri
Page 62 and 63: 218L. F. D. FARACO ET ALLITable I.
Page 64 and 65: 220L. F. D. FARACO ET ALLIBadjeck,
Page 66 and 67: 222L. F. D. FARACO ET ALLIParaná,
Page 68 and 69: Status of Eastern Brazilian coral r
Page 70 and 71: 226Z. M. A. N. LEAO ET ALLIVerrill
Page 72 and 73: 228Z. M. A. N. LEAO ET ALLITable I.
Page 74 and 75: 230Z. M. A. N. LEAO ET ALLICruz (20
Page 76 and 77: 232Z. M. A. N. LEAO ET ALLIdistinct
Page 78 and 79: 234Z. M. A. N. LEAO ET ALLIDutra, L
Page 80 and 81: Temporal and meridional variability
Page 82 and 83: 238Á. M. CIOTTI ET ALLIdistributin
Page 84 and 85: 240Á. M. CIOTTI ET ALLIFigure 2. B
Page 86 and 87: 242Á. M. CIOTTI ET ALLIat the BSC
Page 88 and 89: 244Á. M. CIOTTI ET ALLIcostal upwe
Page 90 and 91: 246Á. M. CIOTTI ET ALLIfrom Area 7
Page 92 and 93: 248Á. M. CIOTTI ET ALLITable III.
Page 94 and 95:
250Á. M. CIOTTI ET ALLICampbell, J
Page 96 and 97:
252Á. M. CIOTTI ET ALLIfloats. Dee
Page 98 and 99:
Regime shifts, trends and interannu
Page 100 and 101:
256FERNANDO E. HIRATA ET ALLIThe st
Page 102 and 103:
258FERNANDO E. HIRATA ET ALLIcompar
Page 104 and 105:
260FERNANDO E. HIRATA ET ALLIUsing
Page 106 and 107:
262FERNANDO E. HIRATA ET ALLIFigure
Page 108 and 109:
264FERNANDO E. HIRATA ET ALLIthis i
Page 110 and 111:
266FERNANDO E. HIRATA ET ALLItal ch
Page 112 and 113:
268D. MUEHE ET ALLIIntroductionThe
Page 114 and 115:
270D. MUEHE ET ALLItrenches were du
Page 116 and 117:
272D. MUEHE ET ALLIging the vegetat
Page 118 and 119:
274D. MUEHE ET ALLIFigure 15. Estim
Page 120 and 121:
276D. MUEHE ET ALLIPetrology, 27: 3
Page 122 and 123:
278A. A. MACHADO ET ALLIdays, it is
Page 124 and 125:
280A. A. MACHADO ET ALLIwas tested
Page 126 and 127:
282A. A. MACHADO ET ALLIthe initial
Page 128 and 129:
284A. A. MACHADO ET ALLIFigure 10.
Page 130 and 131:
286A. A. MACHADO ET ALLIlevel. A ha
Page 132 and 133:
288S. MEDEANIC & I. C. S. CORREAInt
Page 134 and 135:
290S. MEDEANIC & I. C. S. CORREATab
Page 136 and 137:
292S. MEDEANIC & I. C. S. CORREAFig
Page 138 and 139:
294S. MEDEANIC & I. C. S. CORREA(in
Page 140 and 141:
296S. MEDEANIC & I. C. S. CORREAJar
Page 142 and 143:
Representations in the Brazilian me
Page 144 and 145:
300D. HELLEBRANDT & L. HELLEBRANDTT
Page 146 and 147:
302D. HELLEBRANDT & L. HELLEBRANDTF
Page 148 and 149:
304D. HELLEBRANDT & L. HELLEBRANDTc
Page 150 and 151:
306D. HELLEBRANDT & L. HELLEBRANDTT
Page 152 and 153:
308D. HELLEBRANDT & L. HELLEBRANDTB
Page 154 and 155:
Differences between spatial pattern
Page 156 and 157:
312D.F.M GHERARDI ET ALLIface too m
Page 158 and 159:
314D.F.M GHERARDI ET ALLIFigure 3.
Page 160 and 161:
316D.F.M GHERARDI ET ALLIthe Brazil
Page 162 and 163:
318D.F.M GHERARDI ET ALLIAcknowledg
Page 164 and 165:
An essay on the potential effects o
Page 166 and 167:
322F. A. SCHROEDER & J. P. CASTELLO
Page 168 and 169:
Page 170 and 171:
Page 172 and 173:
Page 174 and 175:
Page 176 and 177:
332A. T. LEMOS & R. D. GHISOLFIIntr
Page 178 and 179:
334A. T. LEMOS & R. D. GHISOLFIeros
Page 180 and 181:
336A. T. LEMOS & R. D. GHISOLFITabl
Page 182 and 183:
338A. T. LEMOS & R. D. GHISOLFIFigu
Page 184 and 185:
340A. T. LEMOS & R. D. GHISOLFIOcea
Page 186 and 187:
342M. B. S. F. COSTA ET ALLIcoastal
Page 188 and 189:
344M. B. S. F. COSTA ET ALLIResults
Page 190 and 191:
346M. B. S. F. COSTA ET ALLIlevel i
Page 192 and 193:
348M. B. S. F. COSTA ET ALLIPaulist
Page 194 and 195:
Temporal changes in the seaweed flo
Page 196 and 197:
352CAROLINE DE FAVERI ET ALLITable
Page 198 and 199:
354CAROLINE DE FAVERI ET ALLICallit
Page 200 and 201:
356CAROLINE DE FAVERI ET ALLIcomple
Page 202 and 203:
RIO GRANDE DECLARATION1 st BRAZILIA
Page 204 and 205:
XIVResearchers from Rede Clima and
show all

Download full issue - PanamJAS

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?