Annecy is at the same latitude as Mount Blanc and corresponds with neighboring Chambery warming up of all the seasons 1843-1852, 1773-1842 is cooler, 1843-1913 slightly warmer

Time lag in glacial reactions such as presiding with the Annecy-Chamonix area from 1852-1863 are a meteorological cause separated from the glacial effect by a one decade of inertia. As Annecy series show how Alpine glaciers respond to local climate oscillations, the ical period is a few centuries staid but the meteorlogical character of the Alpine seasons [the Witterungscharakter] differs slightly from what is for the 20th century Alps and Europe in general. Any method between glaciers and temperatures. Without much of a meteorological cause in 14th century water serving mill, a factorial detriment that seized to enterprise inhabitants of French e-Comte, warmed winters partly because of great frosts but in less mild winters, more frequency of frosts. The constitute effect of an inverse symmetrical thermo flux that parallels occurrences after 1850 when winters are milder and frosts less frequent and opening scattered methods between sets of data for correspondences in a tighter magnetism adjoining the metric system and historical years.

The Little Ice Age does not show to involve any significant agricultural effects only in as much, climate deterioration causes growth of neves and glaciers that are factors of cooling down in the microclimate. Viticulture and techniques are relatively fixed as the demand of market consumers changes little over time and stable phonological curves extending over a century synthesizes series for probably attrition. Wine harvests would probably give various titles to climatic fidelity with a positive result or a concordance between vineyards that are close to one another. Such are minima to dendrochronological curves but the warm and cool flux in a season (sagsignatur) or punctuality accounts primary for human factors or increases accumulation and decrease ablation of incomings exceeding outcomings. The medieval climate of intersecular phase in the Alpine glaciers or Fernau oscillation is defined with probable climatic determinants or maximal moraines of Fernau glacier ending in marsh or peat bog of the Bunte Moor with a correspondence to glacial minima. The geomorphologic method and radiocarbon dating alternate strata of peat bog and glacial sand against a time scale.

The O 18 ice sheet memory involving small fluxes in quantity of solar radiation and secular trends of solar activity makes low production of C 14 in warm periods associative of high concentration of O18. As an effect like a consolidated event, the rise of temporal oscillation in uptake of C14 by plants gives phenology a far from long lost contribution to group composition. Climate and Carbon 14concentrations were independently influenced by the unusual quiet state of the sun and periodicity elsewhere into reversions of frequency. Convergence between carbon 14 and Oxygen 18 in contrast with centuries of quiet sun and climate cool down are called the pleasant periods of optima. The 20th century with an amelioration and longer little optimums of the early Middle Ages conclude many assimilatory factors. Without satellites, that is vise a vise, devised sound, and without the visualization of data tables, the increased number of sunspots in the secular long-term by low production of C14 by high production of 018 would be like permeated friction without some other factor.

5 long-term glacial episodes

-/ Fundamental chronological divisions of the post glacial age to the Quaternary - a continuity between historical and geological time / oscillations of geological time that are intersecular, millenary, intermillenary within the subaltantic period forms

Allalin glacier of Saaser Visp valley in Switzerland

[Radiocarbon date of glacial advance in the Alps 1215-1350]

Converging, the Oberriederin, an early irrigation near Aletsch much smaller in the Middle Ages than the 17th century and was abandoned 1385. The fossil forest chronicle at Grindelwald 16th-17th locale with a church movement in 1096 from the Burgbiel as compared to fossil trunks with petrified wood in the Danube under piles of a Roman Bridge

· Peat bog of the medieval thrust - terminus ad quem or terminus ad quo

· Contours of continent- distinct seasoning contributing to the freezing of O-zone then why glacial withdrawal and warm climate last a century