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A northern hemisphere thermodynamic climate\udmodel is used to compute the effect of the insolation anomalies due to orbital\udvariations in the climates for the next 4000 years. Berger's mean monthly\udanomalies of insolation are used in the computations, which are carried out for\ud1000, 2000, 3000 and 4000 years after present (kyears AP). The numerical\udsimulations show that in the climates of the next 4000 years, due to the effect\udof the orbital variations, springs and summers will be increasingly dryer and\udfalls and winters wetter than the present climate

On the seasonal effect of orbital variations on the climates of the next 4000 years