scholarly journals Bioclimatic Approach for Climate Classification of Nigeria

2020 ◽  
Vol 12 (10) ◽  
pp. 4192
Author(s):  
Tolulope Dorcas Mobolade ◽  
Parastoo Pourvahidi
Keyword(s):  
Climate Change ◽  
Vernacular Architecture ◽  
Mechanical Equipment ◽  
Climatic Data ◽  
Climate Classification ◽  
Climatic Regions ◽  
The People ◽  
Harsh Climate ◽  
Cool Climate

One of the fundamental determinants of buildings is the protection of the people who live and work within them from a harsh climate, but a lot of buildings in Nigeria are no longer providing the required comfort needed. The gas emissions through the use of mechanical equipment and lack of energy efficiency in buildings are the major causes of climate change. The way architecture responds to climate change is important. Thus, this research attempted, by using the new bioclimatic chart, to prepare the new climate classification of Nigeria. The research was aimed at establishing a bioclimatically based approach for architecture in Nigeria. By retrieving the climatic data from thirty-six Nigerian meteorological stations about characteristics of each region, bioclimatic analysis was achieved. According to the bioclimatic analysis of this research, Nigeria can be divided into five different climatic regions, such as hot-dry, hot-humid, temperate-dry, temperate-humid, and temperate-dry with a cool climate. We aimed to prove that the climate classification gives the proper answer, dependent upon the vernacular architecture analyzed on Nigeria.

scholarly journals Regularities in species niches reveal the World’s climatic regions

2019 ◽  
Author(s):  
Joaquín Calatayud ◽  
Magnus Neuman ◽  
Alexis Rojas ◽  
Anton Eriksson ◽  
Martin Rosvall
Keyword(s):  
Conservation Planning ◽  
Geographical Information ◽  
Climate Classification ◽  
Climatic Regions ◽  
Evolutionary Studies

Although classifications of the Earth’s climates date back to the ancient Greeks, the climatic regions shaping the distribution of animals remain poorly resolved. Here we present a classification of global climates based on regularities in realised niches of 3657 amphibians, 7204 reptiles, 10684 birds and 4574 mammals. We found 16 main climatic regions that are mostly consistent across groups and previous plant expert-based classifications, confirming the existence of major climatic restrictions for life. The results also suggest that differences among groups likely relate to their particular adaptations and dispersal capabilities. We further show how the integration of species niche classifications with geographical information provides valuable information on potential mechanisms shaping the climatic regions. Our climate classification has applications in several disciplines, including conservation planning and ecological and evolutionary studies.

scholarly journals Climate Scenarios And Your Changes In The Life Zone For Brazil

2021 ◽  
Author(s):  
Rafael Fausto de Lima ◽  
LUCAS Eduardo OLIVEIRA-APARECIDO ◽  
João Antonio Lorençone ◽  
Pedro Antonio Lorençone ◽  
José Reinaldo da Silva Cabral de Moraes ◽  
...  
Keyword(s):  
Climate Change ◽  
Tropical Forest ◽  
Tropical Rainforest ◽  
Potential Evapotranspiration ◽  
Classification Systems ◽  
Annual Precipitation ◽  
Climatic Data ◽  
Climate Change Scenarios ◽  
Historical Series

Abstract Climate classification systems are tools capable of facilitating the analysis, grouping, delimitation, and dissemination of climatic characteristics of a region, contributing to the delimitation of areas of fitness in the agricultural sector and validation of various models of climate change. Thus, we seek to determine life zones for Brazil using the ecological classification of Holdridge (1967) in different scenarios of climate change. A 30-year historical series (1989-2019) of climatic data of average air temperature (° C) and rainfall (mm) was used for the entire Brazilian territory, obtained through the National Aeronautics and Space Administration / Prediction of World platform Wide Energy Resources - (NASA/POWER). Potential evapotranspiration (PET) was estimated by the method of Camargo (1971) using combinations between annual precipitation, average annual biotemperature, average annual basal biotemperature, and the relationship between evapotranspiration and altitude, the life zones for the Holdridge (1967) system were defined. The scenarios used were based on the IPCC (2014) projections. The average temperature in Brazil ranges from 13.1 to 28.0 ° C and the average annual precipitation is 1467 (± 46.91) mm. In the current scenario for the classification of Holdridge (1967) the predominant zone of life is the humid basal tropical forest in 60.57% of the territory. The increase in temperature causes a predominance of the living zones Basal tropical rainforest in 48.92% for S2 and Basal tropical rainforest in 48.95% in S3, the reduction in precipitation S4 generates the predominance of the living zone Basal tropical forest drought in 49.87%, with the increase in precipitation S5 there is a predominance of the zone of life Low humid basal tropical forest in 50.12% of the territory. The great variability of the obtained life zones makes the Holdridge system a useful tool to validate climate change scenarios.

Climate Change Uncertainty and the Classification of 226 Local Entities in Korea

2020 ◽  
Vol 11 (222) ◽  
pp. 507-520
Author(s):  
Jaewan Kim ◽  
Tae Yong Jung ◽  
Chan Park ◽  
Jongwoo Moon ◽  
Dahyun Kang
Keyword(s):  
Climate Change ◽  
Climate Change Uncertainty

Climate Change and Drought: Impact of Food Insecurity on Gender Based Vulnerability in District Tharparkar

2018 ◽  
Vol 57 (3) ◽  
pp. 307-321 ◽  
Author(s):  
Manzoor Hussain Memon ◽  
Naveed Aamir ◽  
Nadeem Ahmed
Keyword(s):  
Climate Change ◽  
Food Insecurity ◽  
Water Scarcity ◽  
Work Load ◽  
Jel Classification ◽  
Arid Ecosystems ◽  
Global Changes ◽  
The People ◽  
Gender Based ◽  
Arid Desert

Climate change has now become a reality that has intensified the sufferings of people living in arid ecosystems. Decrease in rainfall, rise in temperature and increase in the frequency of extreme events are some of the changes observed in the semi-arid desert of district Tharparkar. For thousands of years, people of Tharparkar are coping with drought and aridity of the land by using indigenous knowledge. However, global changes in the climatic pattern and deterioration of social and economic conditions have pushed the inhabitants of this arid region into extreme vulnerable situation. This paper investigates the link between climate-induced natural disasters, particularly drought, from the perspective of changing climate patterns which have resulted in food insecurity and water scarcity. The paper analyses the rainfall pattern in the last 38 years—dividing it into two periods i.e. from 1975-1994 and 1995-2014. The findings of the paper have challenged the prevailing notions about aridity and rainfall patterns in Tharparkar district. The research found that there is an increase in average annual precipitation in the district with erratic patterns. Thus, the nature of drought in the district has changed from its historic pattern of less or no rainfall to more but erratic rainfall that is more threatening to livelihoods of the people that in turn have multiplier effect on water and food insecurity. In particularly, women are more vulnerable in the absence of social security and lack of basic necessities for their survival amidst drought. For instance, traditionally the burden of managing water resources falls on women, which leads to an increased work load during the time of drought and also water scarcity. JEL Classification: Q54, Q56, Q25, I30 Keywords: Climate, Environment and Development, Drought, Water, Poverty

scholarly journals Assessing the Sensitivity of Main Crop Yields to Climate Change Impacts in China

Atmosphere ◽  
2021 ◽  
Vol 12 (2) ◽  
pp. 172
Author(s):  
Yuan Xu ◽  
Jieming Chou ◽  
Fan Yang ◽  
Mingyang Sun ◽  
Weixing Zhao ◽  
...  
Keyword(s):  
Climate Change ◽  
Crop Yield ◽  
Food Production ◽  
Crop Yields ◽  
Climatic Factors ◽  
Climatic Data ◽  
The South ◽  
The North ◽  
Output Elasticity ◽  
The Impact

Quantitatively assessing the spatial divergence of the sensitivity of crop yield to climate change is of great significance for reducing the climate change risk to food production. We use socio-economic and climatic data from 1981 to 2015 to examine how climate variability led to variation in yield, as simulated by an economy–climate model (C-D-C). The sensitivity of crop yield to the impact of climate change refers to the change in yield caused by changing climatic factors under the condition of constant non-climatic factors. An ‘output elasticity of comprehensive climate factor (CCF)’ approach determines the sensitivity, using the yields per hectare for grain, rice, wheat and maize in China’s main grain-producing areas as a case study. The results show that the CCF has a negative trend at a rate of −0.84/(10a) in the North region, while a positive trend of 0.79/(10a) is observed for the South region. Climate change promotes the ensemble increase in yields, and the contribution of agricultural labor force and total mechanical power to yields are greater, indicating that the yield in major grain-producing areas mainly depends on labor resources and the level of mechanization. However, the sensitivities to climate change of different crop yields to climate change present obvious regional differences: the sensitivity to climate change of the yield per hectare for maize in the North region was stronger than that in the South region. Therefore, the increase in the yield per hectare for maize in the North region due to the positive impacts of climate change was greater than that in the South region. In contrast, the sensitivity to climate change of the yield per hectare for rice in the South region was stronger than that in the North region. Furthermore, the sensitivity to climate change of maize per hectare yield was stronger than that of rice and wheat in the North region, and that of rice was the highest of the three crop yields in the South region. Finally, the economy–climate sensitivity zones of different crops were determined by the output elasticity of the CCF to help adapt to climate change and prevent food production risks.

Sustainable Development of Tourism Choice - Eco-Tourism

2013 ◽  
Vol 448-453 ◽  
pp. 4445-4448
Author(s):  
Ming Chong Gu ◽  
Hong Liu
Keyword(s):  
Sustainable Development ◽  
Qualitative Analysis ◽  
Environmental Problems ◽  
Tourism Industry ◽  
Development Model ◽  
The Sustainable Development ◽  
The People ◽  
Domestic Tourism

Along with the development of society and economy, domestic tourism activities is rapidly increased, accompanied by increasing environmental problems brought by the tourism activities is becoming more and more brought to the attention of the people, if our country want to realize the sustainable development of tourism industry, we must replace the old development model to Eco-tourism to meet the needs of tourism and environment. Through qualitative analysis, this paper analyzed the characteristics of the Eco-tourism, and the classification of domestic ecological tourist resources to comb, and put forward some suggestions on developing Eco-tourism, hoping to provide a reference for the development of the domestic Eco-tourism.

A radiocarbon chronology of Holocene climate change and sea-level rise at the Delmarva Peninsula, US Mid-Atlantic Coast

The Holocene ◽  
2021 ◽  
pp. 095968362110482
Author(s):  
Kelvin W Ramsey ◽  
Jaime L. Tomlinson ◽  
C. Robin Mattheus
Keyword(s):  
Climate Change ◽  
North America ◽  
Sea Level Rise ◽  
Sea Level ◽  
Early Holocene ◽  
Eastern North America ◽  
Delmarva Peninsula ◽  
The Holocene ◽  
Cool Climate ◽  
And Sea Level

Radiocarbon dates from 176 sites along the Delmarva Peninsula record the timing of deposition and sea-level rise, and non-marine wetland deposition. The dates provide confirmation of the boundaries of the Holocene subepochs (e.g. “early-middle-late” of Walker et al.) in the mid-Atlantic of eastern North America. These data record initial sea-level rise in the early Holocene, followed by a high rate of rise at the transition to the middle Holocene at 8.2 ka, and a leveling off and decrease in the late-Holocene. The dates, coupled to local and regional climate (pollen) records and fluvial activity, allow regional subdivision of the Holocene into six depositional and climate phases. Phase A (>10 ka) is the end of periglacial activity and transition of cold/cool climate to a warmer early Holocene. Phase B (10.2–8.2 ka) records rise of sea level in the region, a transition to Pinus-dominated forest, and decreased non-marine deposition on the uplands. Phase C (8.2–5.6 ka) shows rapid rates of sea-level rise, expansion of estuaries, and a decrease in non-marine deposition with cool and dry climate. Phase D (5.6–4.2 ka) is a time of high rates of sea-level rise, expanding estuaries, and dry and cool climate; the Atlantic shoreline transgressed rapidly and there was little to no deposition on the uplands. Phase E (4.2–1.1 ka) is a time of lowering sea-level rise rates, Atlantic shorelines nearing their present position, and marine shoal deposition; widespread non-marine deposition resumed with a wetter and warmer climate. Phase F (1.1 ka-present) incorporates the Medieval Climate Anomaly and European settlement on the Delmarva Peninsula. Chronology of depositional phases and coastal changes related to sea-level rise is useful for archeological studies of human occupation in relation to climate change in eastern North America, and provides an important dataset for future regional and global sea-level reconstructions.

Art. VII.—Notes on Persian Belúchistán. From the Persian of Mirza Mehdy Khán. Published Teheran, July, 1875

1876 ◽  
Vol 9 (1) ◽  
pp. 147-154
Author(s):  
A. H. Schindler
Keyword(s):  
Indian Ocean ◽  
Temperate Climate ◽  
The South ◽  
The West ◽  
The North ◽  
The People ◽  
The Indian Ocean ◽  
The Hill ◽  
Cool Climate

The part of Belúchistán now under Persian rule is bounded upon the north by Seistán, upon the east by Panjgúr and Kej, upon the south by the Indian Ocean, and upon the west by Núrámshír, Rúdbár, and the Báshákerd mountains.This country enjoys a variety of climates; almost unbearable heat exists on the Mekrán coast, we find a temperate climate on the hill slopes and on the slightly raised plains as at Duzek and Bampúr, and a cool climate in the mountainous districts Serhad and Bazmán. The heat at Jálq is said to be so intense in summer that the gazelles lie down exhausted in the plains, and let themselves be taken by the people without any trouble.

scholarly journals Soil–landform–plant-community relationships of a periglacial landscape on Potter Peninsula, maritime Antarctica

Solid Earth ◽  
2015 ◽  
Vol 6 (2) ◽  
pp. 583-594 ◽  
Author(s):  
E. L. Poelking ◽  
C. E. R. Schaefer ◽  
E. I. Fernandes Filho ◽  
A. M. de Andrade ◽  
A. A. Spielmann
Keyword(s):  
Climate Change ◽  
Plant Communities ◽  
Terrestrial Ecosystems ◽  
Maritime Antarctica ◽  
Climate Change Effects ◽  
Ornithogenic Soils ◽  
Physical Environmental Factors ◽  
Potter Peninsula

Abstract. Integrated studies on the interplay between soils, periglacial geomorphology and plant communities are crucial for the understanding of climate change effects on terrestrial ecosystems of maritime Antarctica, one of the most sensitive areas to global warming. Knowledge on physical environmental factors that influence plant communities can greatly benefit studies on the monitoring of climate change in maritime Antarctica, where new ice-free areas are being constantly exposed, allowing plant growth and organic carbon inputs. The relationship between topography, plant communities and soils was investigated on Potter Peninsula, King George Island, maritime Antarctica. We mapped the occurrence and distribution of plant communities and identified soil–landform–vegetation relationships. The vegetation map was obtained by classification of a QuickBird image, coupled with detailed landform and characterization of 18 soil profiles. The sub-formations were identified and classified, and we also determined the total elemental composition of lichens, mosses and grasses. Plant communities on Potter Peninsula occupy 23% of the ice-free area, at different landscape positions, showing decreasing diversity and biomass from the coastal zone to inland areas where sub-desert conditions prevail. There is a clear dependency between landform and vegetated soils. Soils that have greater moisture or are poorly drained, and with acid to neutral pH, are favourable for moss sub-formations. Saline, organic-matter-rich ornithogenic soils of former penguin rookeries have greater biomass and diversity, with mixed associations of mosses and grasses, while stable felsenmeers and flat rocky cryoplanation surfaces are the preferred sites for Usnea and Himantormia lugubris lichens at the highest surface. Lichens sub-formations cover the largest vegetated area, showing varying associations with mosses.

Climate change effects on annual streamflow of Filyos River (Turkey)

2018 ◽  
Vol 11 (2) ◽  
pp. 420-433 ◽  
Author(s):  
Adem Yavuz Sönmez ◽  
Semih Kale
Keyword(s):  
Climate Change ◽  
Trend Analysis ◽  
Change Point ◽  
Change Point Analysis ◽  
Climatic Data ◽  
Climatic Parameters ◽  
Annual Streamflow ◽  
Climate Change Effects ◽  
Temperature And Precipitation ◽  
Point Analysis

Abstract The main purpose of this study was to estimate possible climate change effects on the annual streamflow of Filyos River (Turkey). Data for annual streamflow and climatic parameters were obtained from streamflow gauging stations on the river and Bartın, Karabük, Zonguldak meteorological observation stations. Time series analysis was performed on 46 years of annual streamflow data and 57 years of annual mean climatic data from three monitoring stations to understand the trends. Pettitt change-point analysis was applied to determine the change time and trend analysis was performed to forecast trends. To reveal the relationship between climatic parameters and streamflow, correlation tests, namely, Spearman's rho and Kendall's tau were applied. The results of Pettitt change-point analysis pointed to 2000 as the change year for streamflow. Change years for temperature and precipitation were detected as 1997 and 2000, respectively. Trend analysis results indicated decreasing trends in the streamflow and precipitation, and increasing trend in temperature. These changes were found statistically significant for streamflow (p < 0.05) and temperature (p < 0.01). Also, a statistically significant (p < 0.05) correlation was found between streamflow and precipitation. In conclusion, decreasing precipitation and increasing temperature as a result of climate change initiated a decrease in the river streamflow.

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