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Negative commands in Vedic have traditionally been divided into two classes: those built with the Aorist stem and those built with the Present stem The former is said to be "preventive," used to ward off some dreaded future eventuality, while the latter is said to be "inhibitive," used to halt some currently ongoing action. I challenge this division on two grounds: one functional and one formal. Re-examining all prohibitions of the two oldest Sanskrit texts, the Rgveda and the Atharvaveda, I find that there is no correlation between "inhibitive" interpretation and use of the Present stem in Vedic. Having established that the traditional division is incorrect, I then propose a new, formal explanation for the attested distribution of stem types. [ABSTRACT FROM AUTHOR]

In September 2016, militants who were allegedly backed by Pakistan attacked an Indian Army camp in Uri. The government in New Delhi was facing important regional elections. It faced intense public pressure to muster a military response. Such a response, however, ran the risk of triggering a nuclear exchange. Ten days after the Uri attack, India reported that it had carried out 'surgical strikes' on terrorist training camps in Pakistan-controlled territory. The paper examines this specific episode in India–Pakistan deterrence dynamics, focusing on the nomenclature 'surgical strikes'. The paper argues that the choice of the term itself is new and worthy of investigation. Using qualitative content analysis of the official announcement of the operation, it identifies specific rhetorical moves by the Indian government that framed the response as a surgical strike. The paper also considers other statements in the media by high-ranking political and military leaders regarding the strikes, and the reception of these statements by the Indian audience, by Pakistan, and by the international community. The concluding section sounds a note of caution about future iterations of so-called surgical strikes. While the term 'surgical strike' can be useful in some circumstances, it produces destabilising outcomes in others. [ABSTRACT FROM AUTHOR]

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The article discusses the myth of origin from Longterok, which is located in Chungliyimti village, Tuensang district in north-east India. It states that there are two phratries among the Ao Nagas which are the Mongsen dialect speaker Mongsen-ür and the Chongli dialect speaker Chongli-ür. The myth of origin says that Ao Naga ancestors originated from six megaliths at Longterok. Details related to archaeological excavations at Chungliyimti village are also discussed.

This study attempts to find possible linkages between the NCP index and the winter temperature variability over Iran. The investigation is based on statistical analysis of simple, partial and multiple correlations and also evaluation of composite maps of the extreme NCP index and maps of correlation between atmospheric variables and the temperature time series. Our results show that the NCP has a strong negative correlation with the winter temperature in Iran. Furthermore, combination of both the NCP and the AO (Arctic Oscillation) indices improve the correlations in all stations, implying both NCP and AO can be considered as major patterns for explaining the Iranian winter temperature variability. The results show that the positive NCP is associated with enhanced precipitation and cloudy conditions, consequently causing below normal temperature over Iran. The anomalies of OLR in this phase are also negative, implying a cloudy sky. For the negative NCP phase these results are completely reversed. The correlation maps indicate that the NCP is negatively/positively correlated with winter Outgoing Long-wave Radiation/precipitation over Iran. The results also show that the SLP and GPH patterns are quite different for the positive and negative NCP phases over Iran. During the negative NCP a small cyclone is formed over the Arabian Sea causing a strong easterly towards Iran. During the positive NCP this cyclone is removed. Our results show that for the positive NCP years an upper-level trough is formed over northern Iran and the eastern Mediterranean. For the negative NCP years this trough becomes weak and is located over central European regions. This trough is closely linked with the winter temperature over Iran. This is expressed by a high correlation between 500-hPa geopotential height at this region and Iranian winter temperature. [ABSTRACT FROM AUTHOR]