Abstract- The article proposes a hypothesis that is the local warmings in a region impacts the global warming and global climatic changes. The global warming is a common terminology which needs no introduction now. This article introduces the concept of local warming and its effect on local and global climate. This indeed impact the climate change on large. This is the difference in research that lags behind in computation of implications of excess local warmings in a region to same and other places on the planet.
The hypothesis of this article is: The consistent local warming in a region can cause the global impact. Can climatic conditions of a place at times also determine global climatic situations? The suitable reasoning seems to be as follows. The amount of excessive heat in a region can impact the weather on short term and the climate on long term of the surrounding areas. The biggest example of this hypothesis is the Artic and Antarctic ice melting. There is no local warming in these regions, as these regions are primarily not adept to living on by large communities. However, the melting ice shows, that the warmings in other parts of the planet is affecting this region on planet too densely.
The terminology for the local heat produced in the region in this article is called “local warming”. The local warming is defined as the gradual or sudden heating of a region on planet. The boundaries of the region are well defined to be a minimum a city and maximum to a country on whole. These are called city level warmings and country level warmings. Both of these can be considered as the categories of local warmings. The following points explain why local warming of each of these categories are essential to understand. The categories of local warmings are as follows:
- City Level Local Warmings. The city level local warmings are essential to study and this is from where it all emerges. All the heat, change in atmospheric pressure, and ratio of water in air, can be changed and controlled if a city is well planned for its dealing and contribution in local warming statistics. The city level local warmings are the basic building blocks of global warmings and hence an indispensable part of climatic study of global warmings.
- Country Level Local Warmings. The country level local warmings can be measured as a sum total of the local warmings in the key cities of the country. Further, other statistics
Fig 1. Example based illustration of effect of hypothesis of local warmings on global climate change
can be utilized as well in this, which are averaging over top p% of the local warming of regions in a country. The importance of studying country level local warmings is to analyze the way in which this can be reduced and even maintained at current rate. If one knows what is the index of local warming, viz. the statistical marks of the local warming of a country. Then only these things can be controlled well at a global level.
The key topic of discussion here is the consistent local warming over a period of time T and its effect on climatic conditions. The consistent local warming is the warming of a region over a certain period T of time. In this period T the amount of temperature, heat, humidity, quality of air, average atmospheric pressure, location are some of the key points that need to be measured. The amount of heat can be as per hypothesis only increase with time, unless stringent measures are taken. One such measure is de-localization of industrial units and work locations. These should be measured over both the city level global warmings and country level global warmings.
These measurements of the characterizations of local warmings need to be compared with other candidate regions on planets to know which local region stands at which level. And hence which local region is needed to be healed as a climatic emergency. The next section discusses the local warmings and its effect on global levels.
2. Proposed Hypothesis Proof by Illustration
The hypothesis is that local warmings accumulated over a period of time can impact the global warmings. The explanations given here are example based. Consider a region R1 and Region R2, R3 at a distance s1 and s2 from R1. Then for a consistent local warming in a region R1 shall affect the local weather and hence climate over the longer intervals of time. The consistency in change in climate in neighboring regions, as per hypothesis, can be evident. This can be illustrated with help of Figure 1.
In Figure 1, it is elaborated that if there is an excess of consistent local warmings in region R1 this shall affect the climatic conditions at regions R2 and R3. Further this is shown in Figure 1, that region R3 which is furthest from the main area of consistent local warmings can be impacted by climatic changes at region R1 and also by the accumulated climatic changes at region R2 (R2 is itself impacted by R1). Hence R3 is more impacted by local warmings at R1 than R2.
The article presents a hypothesis, and provides the significance of the hypothesis. Further, example-based illustrations are being provided in this article. These are example-based illustrations and formal mathematical proofs are being worked out. More intense proofs are required to prove the hypothesis.
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