Greissan - Aosta region ---The C 14 curve is a question as to whether history is indebted to nuclear physics. And material like multisecular wood samples redeemed from dendrochronologyical cross sections reflect dates within a yeare by tree rings. Having to reflect in some way if not for a glacier, en masse a semi-permeable body is still composite of theory of the greenhouse effect. In simple terms, the reduction of one of its transitory states is transparent to solar raditation. That is a partially opaque paradox of itself radiated back to space from earth. Any linear movement against gravity would link plots but as a heat trap, the stratosphere and temperature are however a metric device. The curve of C14 like a contra mnemosyne is at a hypothetical stage of the decision. Also called a mild optimium phase for the greater of neutrality, independent techniques of many others referenced to stays for quite a while overtime.

The natural radiocarbon product from yeare series 1000-1200. Mini's followed by a rise and then a max like 1500-1700 yeare series have a quality of fresh decline and slow regression up to 1950. Radicarbon production in this time doesnt fall to low levels of the 11 th century or a mild optimum phase. The obergurgler glacier in the recent yeare 1962 brought together a symposium of variations existing and was called the fundamental res conference. Bertin and Recurant in Ecole des Hautes Etudes decided somewhere to concentrate on 2 particular centuries to extend beyond the generalities to the concrete realm of situant history. The short term chronology was ciphered as a paleoclimate rather than a constellation, making it a biograph of geological time also derived from archives of historian provinces. The general and linear connection between both, when a factor decision would be judged would be detrimental to either of primary groups but instead Godard and Nigond, about phenological data relieved the correlation of spring temperatures and flower dates leaving no ceremonial significance to archiving data belonging to the heliothermic complex. This complex accounts for the length of time taken by staples to ripen. No matter where any place, yielding to timing however, the spring debacle of giantic complacency in certain ways could illustrate the elemental use of 3-curves tending to diverge toward thawing or results of amelioration on the contrary. The example of grapes from yeare series 1880-1950 was a lot like the Riga series of 1530-1610 to unearth a few gaps without interacting rates.

The chronological sequence of hard winter after 1550 probes a parallel in the more recent meteor history. The meteor period appears on all meteor series for all the temperate zones having preceded earlier temperature curves for 1900-1950. The history of medieval climate put hard winters from 1550-1600 in the contemporary era of the same meteor family because series of cold years harm agriculture without impacts between the 2 extremes. Excluding interactive human factors, temperature isolates would not affect any index. Temperate Europe has the same recurrence of years with high humidity. Both oceanic concerns divide seriation evenly but not dates in history. The distinction of agricultured meteorology are finite and existing between physical climate and human history - the methods do not always connect and at least partially concede to secular fluctuation or some other major episode in human history and one of them being migratory and longer in the phase of depressed or expanding gradient.

Lassitude contributing to the period of the 17th century and for 1000 is the stimulated quandry as to whether or not the great land clearance of the west revives as state of arbitrary climatic influence. Whether or not, the Teuton trend of leaving the solid cold for mild climate , similtaneous population growth - meanwhile stimulating agriculture was for the greater of the cultural region, predominately responsible for Scandanavian male warriors and departure of surplus. The oscillations similary coincides with phases of the Fernau and recording patterns of climate that are more complex according to season. Usually basin rain and its decisive role in final yields were much more abundance in Mediterranean literary tradtions. With plenty of ripe-here-sowing-there, some harvests as compromised by seasonal weather is insufficient to amount of cultivated favoritism and thus referring heavily to Sein-e-et-Oise i.e, winter conditions in a definite ic order.

Loire- Atlantique rainfall rise above the summer median during the summer and up to harvest enough to make the harvest an epoch of absolute poor and so in condition of winter and spring favorability. Why? wheat trouble. Wheat rots with summer rain and gives not so much as a higher grain yield to England. The paveway of great famines typical of middle ages do not start with Mesopotamia, unless wheat is the center of marked temperatures correlated according to harvests. Limiting factors in cereal geographically according to region is legend for adverse climate conditions that are nowhere near the same for the north of the Baltic, Meditteranean shores, and temperate zones in between. The changing distribution of air masses and jet streams are current to theory of general atmospheric circulation. Concurrent by the means of synoptic maps, anticyclones contrast betweeen known existing situations at the end of the 16th century and its many advancing glaciers with prayer series set aside for drier years and desertification as in the southwestern U.S. With an array falling into a wider span of mechanism applied, many thousands of scattered climatic references to unpublished ificatory groups relate to one another and are subtlties possible to the domain of modern electronics and is a reason adieu to any errs of human consequence that only meteorlogy computerized is related to sustenance between climatic and human history.

Cereal yields contrary to Mediterranean yields in north countries are simple to impact the chiefest operative factor which is temperature and strictly gooder harvests belonging to hottest summers. The later group are most exactly known and while C14 is suggestive for chronos for glaciers, the loose material on only a particular series of seasons, quantify as early and as late for the 11th century [Nile hydrology and U.S dendrology] in apparent order that climatic zones are related to one another and yet far away from each other in possible cross reference. The minimum of fact turns fo influence of climate on activity and ecos that are human in impact. The climate pricing for staples from far away have a based scheme on year-harvest and bring about a lot of subtle consequence to temperate zones as though the context of series that are not subdivided as compared to another series a region lacks chronological precision with no systematic conclusions to series that numerate effects from the most complex, unproved causes, derived hypothesis that marked series at all can keep up with a complementary degree of consequential subtlties. The narrowness of the range brought to the microscope is an electronic attribute and not a substitute for the operant factor. As for secular temperature, variations and autonomy of human phenomenon coincide with them in time and present useless impossibilities of causal links between claims happening to linger without symmetry.

The long term demographic trend among local climatic fluctuation and related centuries are astronomical to both archaic informal human trends and dendrochronological oscillation in humidity as a deterring generality about certain comparisons made between 2 series and crossing over through their variablitiy, the conceivability about the 2 series as in deep space before the modern era. One is a great drought, many groups of trees covering a very long span and the application of a technique such as irrigation and season devised episode for saturation level. Since channels or arroyos recieve the bog effect of lept benefits from canyons above, soil erosion from primary land clear, having temporary channels formed and short term vivisection, the patterns of centuries 17th-20th and the glaciers from Iceland and Alaska advance and retreated to give the bodies a widening thresh for their very own history and revealed sequences in data series or synoptic history of the atmosphere where the grain of element exist in 3-d space and harder sects of phase

Atlantic optimum	1000 A.D
Subatlantic pessimism of Iron Age	500 B.C.E
Pessimism of Modern Era	1200 A.D	culminates Little Ice Age
Cold phase	1550-1700 A.D	intensity of cold - physical ~ binomial interrater
European Pessimism	1690 A.D	defines westerly flow of temperature zone and circular movements of 40th-70th parallels, west to east [The Great Zonal Circular Movement] with parallel lines of latitude and particles that encircle the earth like a ring
currents pass over to Scandanavia, Scotland, Denmark, Baltic / the geom. gradient of affecting the latitudes of depression treks at sea level are displaced +/- toward north and south, east and west, oscillating according to yeare or century or climate type that prevail past more permanent regions - certainty glaciers oscillate

The westerly flow becomes affected at a higher altitude involving the upper westerlies. If easterlies, then cyclonic and equatorial direct. The movement of the upper westerlies northward become stronger and intenser in swiftness and the drive twoard a continental increase of warmth, humidity, oceanic influence; most nominal where oceans and sky meet. A continental influence prevail over an ocean such one. The upper westerlies have structural changes to affect geographic distribution in their characteristic features so that a salty withdrawl throughout levels of the stratosphere produce a system of warm ridges, cold troughs, and compound tography of the surface.

The number of cold troughs widen the area of the continent proportionately to the temperate latitudes of the northern hemisphere and the troughs as a system of typical pessimism and solid regional piece of the Little Ice Age at the end of the 16th and into the 17 centuries, leave behind questions of divergence. Since what affects the westerlies are variations in the temperate zone, structural sustenance of the microbiologies heed with a far ranging complexity. Models of historical climate may be derived for varations but then again, lack of symmetry questions the central purpose of complexity joining together in a climate which is already reduced to two main types.

The existence of 2 types of circulation embodies outward concentrations and may alternate between the 2 circularities, an enabling variation of climate with explanans on every scale in every age which refers to illustration when most materials are more directly. (Hoinkes) example of meteorlogical situations or grosswetterlagen for Central Europe considers lthe recent regression of Alpine glaciers resulting in dual phenomenon affecting summer or else the anticyclonic situations with higher temperature and insolation because frequency during summer after 1930 for the same period brought cyclonic situations with snowfall. The discreetness according to (Pedelaborde) replaces the series of decision diffusively for the acuity at one point and links that are begotten from the atmospheric model outer bodies in space. The compromise of ocean meeting sky in the sphere does not cause either to rise but the projective level of observation confers what is called contrasting Model I and Model II: