Javascript must be enabled to continue!
Insolation Regime of Interglacials
View through CrossRef
Seasonal changes in the extent of snow cover and pack-ice were analysed in the satellite-derived maps of the Northern Hemisphere obtained during the last 5 yr. Two intervals were studied in detail: summer 1968 to summer 1969 and summer 1971 to summer 1972. These studies demonstrate that the variation in ground albedo as a result of changing snow and ice cover affects the Earth's energy budget to a far greater degree than any possible extraterrestrial mechanism could do on such a short time scale. However, the rapid expansion of snow cover between late September and November suggests possible feed-back process which could be speeded up or slowed down by minute changes in energy and moisture budget at the snow accretion area. These changes may be of any origin, natural or artificial, and on the time scales ranging from days to millenia.In this context, the close correspondence between the radiometrically dated gross climate changes within the past 150,000 yr and between the curve showing the rate of change in winter insolation for the middle latitudes of the Northern Hemisphere is conspicuous. The periodicity of about 20,000 yr is involved.An insolation chronology is introduced here, which is based entirely on astronomic factors (on the so called Milankovitch mechanism of Earth orbital elements). It is independent of any geologic or geochronologic dating systems. Two alternating units comprise the insolation chronology.The positive insolation regime (PIR)is an episode defined by progressively increasing winter irradiation in the Northern Hemisphere, whereas thenegative insolation regime (NIR)is an episode of progressively decreasing winter irradiation. ThePIRclosely correlates with the generally warm intervals such as interglacials and temperate interstadials, theNIRwith generally cold intervals. This basic pattern interferes with short-term oscillations which may retard or advance the climate response on the scale of centuries.It is observed that the positive insolation regime designated asPIR110, which started at 11,000 YBP, has ended recently. The new negative insolation regime,NIR 0/ + 8, will last for the next 8000 yr. Inasmuch within the last radiometrically dated 150,000 yr noNIRis known to correlate with generally warm interval, the prognosis is for a long-lasting global cooling more severe than any experienced hitherto by civilized mankind.
Title: Insolation Regime of Interglacials
Description:
Seasonal changes in the extent of snow cover and pack-ice were analysed in the satellite-derived maps of the Northern Hemisphere obtained during the last 5 yr.
Two intervals were studied in detail: summer 1968 to summer 1969 and summer 1971 to summer 1972.
These studies demonstrate that the variation in ground albedo as a result of changing snow and ice cover affects the Earth's energy budget to a far greater degree than any possible extraterrestrial mechanism could do on such a short time scale.
However, the rapid expansion of snow cover between late September and November suggests possible feed-back process which could be speeded up or slowed down by minute changes in energy and moisture budget at the snow accretion area.
These changes may be of any origin, natural or artificial, and on the time scales ranging from days to millenia.
In this context, the close correspondence between the radiometrically dated gross climate changes within the past 150,000 yr and between the curve showing the rate of change in winter insolation for the middle latitudes of the Northern Hemisphere is conspicuous.
The periodicity of about 20,000 yr is involved.
An insolation chronology is introduced here, which is based entirely on astronomic factors (on the so called Milankovitch mechanism of Earth orbital elements).
It is independent of any geologic or geochronologic dating systems.
Two alternating units comprise the insolation chronology.
The positive insolation regime (PIR)is an episode defined by progressively increasing winter irradiation in the Northern Hemisphere, whereas thenegative insolation regime (NIR)is an episode of progressively decreasing winter irradiation.
ThePIRclosely correlates with the generally warm intervals such as interglacials and temperate interstadials, theNIRwith generally cold intervals.
This basic pattern interferes with short-term oscillations which may retard or advance the climate response on the scale of centuries.
It is observed that the positive insolation regime designated asPIR110, which started at 11,000 YBP, has ended recently.
The new negative insolation regime,NIR 0/ + 8, will last for the next 8000 yr.
Inasmuch within the last radiometrically dated 150,000 yr noNIRis known to correlate with generally warm interval, the prognosis is for a long-lasting global cooling more severe than any experienced hitherto by civilized mankind.
Related Results
Local insolation dominates the global land monsoon precipitation on orbital timescales
Local insolation dominates the global land monsoon precipitation on orbital timescales
Orbital-scale monsoon variability exhibits a strong response to orbital insolation forcing. However, previous studies attributing monsoon behavior to either local insolation from t...
Arctic Amplification through Inter-seasonal Feedback Effect in Past Interglacials 
Arctic Amplification through Inter-seasonal Feedback Effect in Past Interglacials 
<p>Past interglacials allow investigating the climatic processes and associated feedbacks during warm periods, which are characterized by different combinations of cl...
The role of eccentricity in determining the spacing between interglacials
The role of eccentricity in determining the spacing between interglacials
<p>In a recent paper Tzedakis et al (2017) described a simple rule that predicts, using only caloric summer half-year insolation as input, which insolation cycles lea...
Asian-Australian monsoon variations at orbital scales – insights from model simulations
Asian-Australian monsoon variations at orbital scales – insights from model simulations
<p>The Asian-Australian monsoon system is mainly composed of East Asian monsoon, Australian monsoon and South Asian monsoon. The Australian monsoon and East Asian mon...
OS SERVIDORES PÚBLICOS MUNICIPAIS
OS SERVIDORES PÚBLICOS MUNICIPAIS
I. Organização do funcionalismo municipal1. A Autonomia dos Municípios e a organização de seu funcionalismo — A Constituição Federal assegura, aos Municípios, a autonomia de autogo...
Carbon cycle dynamics during recent interglacials
Carbon cycle dynamics during recent interglacials
Abstract. Trends in the atmospheric concentration of CO2 during three recent interglacials, the Holocene, the Eemian and Marine Isotope Stage (MIS) 11, are investigated using an Ea...
Different AMOC Stabilization between Past Interglacials and Future
Different AMOC Stabilization between Past Interglacials and Future
The excess freshwater in the Arctic due to global warming is causing a weakening the Atlantic Meridional Overturning Circulation (AMOC). The question of how the climate change will...
The thermal environment of comet 67P/Churyumov-Gerasimenko
The thermal environment of comet 67P/Churyumov-Gerasimenko
Comets are among the most primordial objects of the solar system. According to Davidsson et al. (2016), they did not suffer from collisional processing, and remained mostly thermal...

