Answer:
It will be at 34 ºF
Explanation:
If we start at 12 am with a temperature of 44 ºF, and each hour later, the temperature will be 2 ºF less, so...
1 am - 42 ºF
2 am - 40 ºF
3 am - 38 ºF
4 am - 36 ºF, that is the temperature of the dewpoint.
So after this point, each hour the temperture will decrease 1ºF, so..
5 am - 35 ºF
6 am - 34 ºF, ending with this temperature at the morning.
Hope this info is useful.
Guangzhou 113°E 23°N
shanghai 121°E 31°N
so the direction is northeast
The Hinduism is a religion that is very flexible, very tolerant, and it has managed to exist for several thousands years now. The reason why this religion is like this is that its foundations are based on the merging of two totally different religions. The Hinduism is a mixture of the beliefs of the Dravidians that were one of the first inhabitants of India, and the beliefs of the Aryan people that migrated from Central Asia and integrated into the society. The two groups engaged into sharing of ideas and mutual assimilation, resulting in the rise of the Hinduism, and the caste system with it. Being a religion that has roots in two totally different ancient cultures had made the religion very tolerant to regional and local variations being implemented into it. It can be said that one of the implications of this is that the Hinduism, apart from its basis, has thousands of different variations among its followers. Some variations occur in certain regions, some even on local level, or even in a single village. Over time this can cause problems because the variations of it may start to diverge too much and the religion to split up. On the positive side, it seems that this way of practicing the Hinduism had not actually created any problems throughout its existence, thus for several thousands of years. It seems that the religions is so open to implementing new things in it,and the people to modify it as they feel, that no inner-religious conflicts occur because of it. A disadvantage may be that the Hinduism may lose its core over time, resulting in confusion among its followers.
<h2>Answer</h2>
<h3>This paper traces the history of human-environment interactions in the Pacific Islands during the last millennium, focusing on three main periods: the Little Climatic Optimum, the Little Ice Age, and, in greatest detail, the transition around A.D. 1300 between the two. The Little Climatic Optimum (approximately A.D. 750–1300) was marked by warm, rising temperatures, rising sea level and probably increasing aridity. The latter condition was linked to development of water-conservatory strategies (agricultural terracing being the most common) requiring cooperation between human groups which facilitated formation of large nucleated settlements and increased sociopolitical complexity. The transition period (approximately A.D. 1270–1475) involved rapid temperature and sea-level fall, perhaps a short-lived precipitation increase. Temperature fall stressed crops and reef organisms, sea-level fall lowered water tables and exposed reef surfaces reducing their potential as food resources for coastal dwellers. Increased precipitation washed away exposed infrastructure. Consequently food resource bases on many islands diminished abruptly across the transition. The Little Ice Age (approximately A.D. 1300–1800) was marked by cooler temperatures and lower sea levels. The lingering effects of the earlier transition largely determined human lifestyles during this period. Conflict resulted from resource depletion. Unprotected coastal settlements were abandoned in favour of fortified inland, often upland, settlements. Climate change is suggested to have been a important determinant of human cultural change during the last millennium in the Pacific Islands.</h3>
<h2>Journal Information</h2>
<h3>Environment and History is an interdisciplinary journal which aims to bring scholars in the humanities and biological sciences closer together, with the deliberate intention of constructing long and well-founded perspectives on present day environmental problems.</h3>
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<h2>Rights & Usage</h2>
<h3>This item is part of a JSTOR Collection. </h3><h3>For terms and use, please refer to our Terms and Conditions </h3><h3>Environment and History © 2001 White Horse Press </h3><h3>Request Permissions</h3>
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