FREE BOOKS

Author's List




PREV.   NEXT  
|<   262   263   264   265   266   267   268   269   270   271   272   273   274   275   276   277   278   279   280   281   282   283   284   285   286  
287   288   289   290   291   292   293   294   295   296   297   298   299   300   301   302   303   304   305   306   307   308   309   310   311   >>   >|  
ing south of the tropic of Capricorn. In general terms, it is a tropical country, with sub-tropical and temperate areas covering its three southern states and a great part of the elevated central plateau. The forest-covered, lowland valley of the Amazon is a region of high temperatures which vary little throughout the year, and of heavy rainfall. There is no appreciable change of seasons, except that produced by increased rainfall in the rainy season. The average temperature according to Castelnau is about 78 deg.F., or 82.40 deg. to 84.20 deg. F. according to Agassiz. There is an increase in the rainfall from August to October, and again from November to March, the latter being the regular rainy season, but the time varies considerably between the valley of the upper Amazon and those of the upper Madeira and Negro. There is usually a short dry season on the upper Amazon in January and February, which causes two annual floods--that of November-December, and the great flood of March-June. The subsidence of the latter usually lasts until October. The average rainfall throughout the whole Amazon valley is estimated by Reclus as "probably in excess of 2 metres" (78.7 in.), and the maximum rise of the great flood is about 45 ft. The prevailing winds in the Amazon valley are easterly and westerly (or south-westerly), the former warm and charged with moisture, the latter dry and cold. The easterly winds, which are deflections of the trade winds, blow upstream with great regularity and force, more especially in the winter or dry season, and are felt as far inland as the mouths of the Madeira and Negro. Above these they are less regular and are attracted northward by the heated _llanos_ of Venezuela in winter, or southward by the heated _campos_ of Matto Grosso in summer. The cold south-westerly winds are felt when the sun is north of the equator, and are most severe, for a few days, in the month of May, when a _tempo da friagem_ (cold period) causes much discomfort throughout the upper Amazon region. There are winter winds from the Andes, but in the summer season there are cold currents of air from up-river (_ventos da cima_) which are usually followed by downpours of rain. The coastal plain as far south as Santos is a region of high temperatures and great humidity. The year is usually divided into a winter (_inverno_) and summer (_verao_), corresponding appr
PREV.   NEXT  
|<   262   263   264   265   266   267   268   269   270   271   272   273   274   275   276   277   278   279   280   281   282   283   284   285   286  
287   288   289   290   291   292   293   294   295   296   297   298   299   300   301   302   303   304   305   306   307   308   309   310   311   >>   >|  



Top keywords:
Amazon
 

season

 

valley

 

winter

 

rainfall

 

westerly

 

summer

 

region

 

October

 
average

tropical

 

Madeira

 

November

 

regular

 

easterly

 

heated

 

temperatures

 
upstream
 
llanos
 
regularity

attracted

 

inland

 

mouths

 

moisture

 

charged

 

deflections

 

northward

 

downpours

 
ventos
 

currents


coastal
 
inverno
 

Santos

 
humidity
 
divided
 
equator
 

prevailing

 

severe

 
Grosso
 
southward

campos
 

period

 

discomfort

 
friagem
 
Venezuela
 

January

 

lowland

 

plateau

 

forest

 

covered