Model I

is a type of period of circulation with modified upper westerlies structure, clause troughs close enough together that the shift west i.e., from East Europe to over Europe reedeems altitude through movement

The increased frequency during the Little Ice Age centuries reputes the incursions of cold air from the north into the south from Sea of Norway down to the Western Mediterranean
  • dispersed throughout the equator and predominates during cooling down pessimisms
  • the displacement southward in the summer 57 degree through 60 degree north like the bad decades famously from 1590s-1690s- passing south and over Scotland and Denmark 50 degree through 60 degree North / there were 8/10 summers in between, lessening the energy and general weakening of pressure gradients in the mainstream
  • westerlies form a part of a general system of transfer of warm air from the tropics to the polar zone with loss of force implying weakened transport of heat and moisture or "bogging" of polar regions in the presence of a cool factor of major importance in high, temperate latitudes.
  • a type of circulation spreading out southward with comparative lack of intrinsic energy acts with narrow trough pattern of crowding together and thwarting carried from leverage tending to the west in the upper westerlies
  • correlations of interrelated factors with periods of cooling and pessimism in N. America and Europe

 

Model II

...result of dual phenomenon of Alpine glaciers affecting summer similar complexity to the anticyclonic high temp. situations- the frequency of season before and after a technical yeare of the same period describing cyclonic situations.

 

  • Increased albedo became predictively in a set series ongoing, correspondingly fewer / ic anthropic principle
  • characteristic of warming up abstract force in the equation of the optimum early or recent
  • The whirl or circumpolar vortex of westerlies spreads out to the equator to contract around the pole with depression tracks mostly northerly.
  • summers are hotter and brighter as passing cyclones to the north and Western Europe are more under the influence of southern anticyclones- may contrast with stark matter reflective of westerlies
~~winters growing warmer periodically with intensified circulation contrary to different levels in the atmosphere~~
  • dissolving periodicity with cooler heights and warmer ocean and moisture to Western Europe- effective summer
  • more zonal , trough ridge pattern of upper atmospheric circulation product change converse to what what Mod. I produce
  • 1890-1950 culminating of recent amelioration: oceanic and zonal warming up, decimal elements of less frequency, cold breakout resulting in a general rise in mean temperatures producing intense fusion of glaciers
  • main features of synoptic situations in the temperate zone and introductive unity into climate and history interpretation