﻿336 
  0. 
  L. 
  Fassig 
  — 
  March 
  Weather 
  in 
  the 
  United 
  States, 
  

  

  the 
  West 
  Indies 
  througli 
  the 
  Gulf 
  of 
  Mexico, 
  npthe 
  Mississippi 
  

   Valley 
  and 
  across 
  the 
  Lake 
  region. 
  The 
  Atlantic 
  high 
  area 
  

   extended 
  far 
  to 
  the 
  west 
  of 
  its 
  usual 
  position. 
  Similarly 
  the 
  

   conditions 
  for 
  September, 
  1883, 
  were 
  charted, 
  during 
  which 
  a 
  

  

  

  140 
  120 
  

  

  100 
  

  

  80 
  

  

  60 
  

  

  4 
  

  

  

   60 
  

  

  60 
  

  

  

  SiD.2 
  /// 
  

  

  .//m 
  

  

  *f^^ 
  

  

  ^^><0^/ 
  

  

  

  w^'^ 
  

  

  

  ^^\?^ 
  

  

  

  y^k 
  

  

  ^^M/ 
  

  

  rf 
  

  

  AK^ 
  

  

  

  % 
  

  

  

  

  vy^ 
  

  

  ^^^ 
  

  

  XTy/// 
  

  

  ^^^ 
  

  

  

  

  

  ^^5:> 
  

  

  

  

  

  M 
  

  

  » 
  

  

  

  ^ 
  

   K 
  

  

  ^ 
  

  

  S 
  

  

  l^ 
  

  

  O 
  

  

  V 
  

  

  

  

  40 
  

  

  

  ^W0? 
  

  

  yw//yT/ 
  

  

  

  

  <*?s^^ 
  

  

  ^^^ 
  

  

  

  \ 
  ^ 
  

  

  .^ 
  

  

  40 
  

  

  

  +^°'"^^ 
  

  

  ^^^ 
  

  

  \ 
  

  

  

  ^^^ 
  

  

  ^^^ 
  

  

  

  

  

  

  

  ^<2 
  

  

  ^^ 
  

  

  w)\ 
  

  

  

  ^^ 
  

  

  ^ 
  

  

  

  zoa 
  

  

  

  

  20 
  

  

  

  

  % 
  

  

  4hi 
  

  

  \\ 
  

  

  ^m 
  

  

  ^ 
  

  

  ^ 
  

  

  

  

  20 
  

  

  

  

  N 
  

  

  

  ^c 
  

  

  ^:^ 
  

  

  

  

  L 
  

  

  ■l^ 
  

  

  ^Q 
  120 
  

  

  100 
  

  

  , 
  8 
  

  

  

  

  lo 
  

  

  40 
  

  

  March, 
  1885. 
  

  

  West 
  Indian 
  hurricane 
  took 
  a 
  path 
  farther 
  to 
  the 
  eastward 
  

   than 
  usual. 
  The 
  Atlantic 
  high 
  area 
  was 
  well 
  to 
  the 
  east 
  of 
  its 
  

   usual 
  position. 
  In 
  both 
  cases 
  the 
  path 
  of 
  the 
  hurricane 
  was 
  

   along 
  the 
  western 
  edge 
  of 
  the 
  Atlantic 
  high 
  area. 
  

  

  