Nanda Rajjat Yatra

Nanda Devi Raj Jaat Yatra is celebrated in Uttarakhand which is known as the abode God. Nanda Devi is considered as the fundamental god in this wonderful and spiritual place. She is accepted to have been the life partner of Lord Shiva and the little girl of the leader of the mountains. Both Kumaon and Garhwal locales in Uttarakhand worshp Nanda Devi; in reality the Yatra is a standout amongst the most celebrated religious occasions in India. Nanda Devi Raj Jaat Yatra is celebrated every 12 years in Uttarakhand. This holy Yatra include a long course that takes twenty two days for fulfillment. The devotee travels almost 280 kilometers by trekking.
The Nanda Devi Raj Jaat offers an unmatched ordeal to the travelers, especially for those who have an interest in religious traditions and the local culture of Uttarakhand. Its sacredness for local people is the same to that of the Kumbh. Nanda Devi Raj Jat Yatra is considered as a standout amongst the most vivacious and brilliant celebrations in the region. The holy yatra starts from Nauti town in Karanprayag and goes through the lifted icy pool of Hemkund. The shimmering Hemkund Lake is roosted at a height of 3832 meters above ocean level. The course to reach here is by means of Roopkund Lake, which is otherwise called a secretive lake. The sacred tour of Nanda Devi Raj Jat is held to go with Nanda Devi to Lord Shiva's home.

History of Nanda Devi Raj Jat Yatra

The legend behind the Yatra is that Nanda Devi, Lord Shiva�s wife, went away to Nanda Devi Parbat. When the Yatra starts, heavy rain is expected as it is believed that the tears of Goddess Nanda rolls down in the form of rainfall. The Nanda Devi Festival supposedly started during the 16th century and is highly popular in the Nauti, Almora, Nainital, Munsiyari and Ranikhet regions. It is said that the Devi visits her maternal home in Bhado (to some degree around the months of August). The visit of the goddess is celebrated by the nearby environments as a period of celebration.

Registration for Nanda Devi Raj Jat Yatra

As indicated by the representative speaker of Uttarakhand Vidhan Sabha, Mr. A.P. Maikhuri, the enlistment procedure of the enthusiasts willing to go for Shri Nanda Devi Raj Jat Yatra will incorporate a medicinal examination. Just the individuals who breeze through this restorative test would be permitted to go on the Yatra. A measure of 150 crore rupees was apportioned by the state legislature of Uttarakhand, for the development of extensions and streets for the consecrated adventure of Raj Jat.

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Weather / Climate in Nanda Rajjat

As the elevation of the district ranges from 800 mts. to 8000 mts above see level the climate of the district very largely depend on altitude. The winter season is from about mid November to March. As most of the region is situated on the southern slopes of the outer Himalayas, monsoon currents can enter through the valley, the rainfall being heaviest in the monsoon from June to September.

Rainfall -

Most of the rainfall occur during the period June to September when 70 to 80 percent of the annual precipitation is accounted for in the southern half of the district and 55 to 65 percent in the northern half. The effectiveness of the rains is, among others, related to low temperature which means less evapo-transpiration and forest or vegetation cover. However, the effectiveness is neither uniform nor even positive in areas where either the vegetational cover is poor or / and has steep slopes or the soils have been so denuded that their moisture absorption capacity has become marginal.
Rain gauging stations put up at seven locations by Meteorological department of Govt. of India, represent the settled land mass of Chamoli district.

Temperature -

The details of temperature recorded at the meteorological observatories in the district show that the highest temperature was 34 ℃ and lowest 0 ℃. January is the coldest month after which the temperature begin to rise till June or July. temperature vary with elevation. During the winter cold waves in the wake of western disturbances may cause temperature to fall appreciably. Snow accumulation in valleys is considerable.

Humidity -

The relative humidity is high during monsoon season, generally exceeding 70% on the average. The driest part of the year is the pre monsoon period when the humidity may drop to 35% during the afternoon. During the winter months humidity increases toward the afternoon at certain high stations.
Cloudiness - Skies are heavily clouded during the monsoon months and for short spells when the region is affected by the passage of western disturbances. During the rest of the year the skies are generally clear to lightly clouded.

Winds -

Owing to the nature of terrain local affect are pronounced and when the general prevailing winds not too strong to mask these effect, there is a tendency for diurnal reversal of winds, the flow being anabatic during the day and katabatic at night, the latter being of considerable force.

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