Diurnal thermal diversity in heterogeneous built area: Mumbai, India

Urban Climate ◽  
2020 ◽  
Vol 32 ◽  
pp. 100627 ◽  
Author(s):  
Surabhi Mehrotra ◽  
Ronita Bardhan ◽  
Krithivasan Ramamritham
Keyword(s):  
2020 ◽  
Vol 29 (9) ◽  
pp. 1486-1494 ◽  
Author(s):  
Jelena Bujan ◽  
Karl A. Roeder ◽  
Kirsten Beurs ◽  
Michael D. Weiser ◽  
Michael Kaspari

Notions of batholith magma generation in crustal thermal environments are countered by the consanguinity of intrusive and extrusive magmas at destructive plate margins, their overlapping mantle-type initial strontium isotope ratios and by their contribution to observed crustal thickening in the absence of significant shortening. Conductive heat modelling produces geotherms which do not intersect the field of crustal fusion. However, crustal scavenging by ascending melts, initiated in the mantle, is a distinct possibility in most tectonic environments. Scavenging occurs more effectively at modern plate margins as activity continues to increase crustal thicknesses, temperatures and acidity of magmas. However, evidence from British Caledonian granites, an older Cordilleran suite, shows the opposite crustal cooling trend probably linked to younger granite formation after subduction processes ceased. Mantle derived Cordilleran magmas contribute to contemporary crustal growth at 0.1—0.5 km 3 a -1 - a decreasing rate, proportional to the Earth’s decaying thermal output, which has controlled the changing style of tectonics and granitic activity during geological history.


River Science ◽  
2016 ◽  
pp. 259-278
Author(s):  
Jack A. Stanford ◽  
Michelle L. Anderson ◽  
Brian L. Reid ◽  
Samantha D. Chilcote ◽  
Thomas S. Bansak

2020 ◽  
Vol 56 (4) ◽  
pp. 630-646 ◽  
Author(s):  
Rebecca Shaftel ◽  
Sue Mauger ◽  
Jeff Falke ◽  
Daniel Rinella ◽  
Jeff Davis ◽  
...  
Keyword(s):  

2020 ◽  
Vol 3 (1) ◽  
pp. 74
Author(s):  
Longina Chojnacka-Ożga ◽  
Wojciech Ożga

In recent decades, relatively few experimental studies have been carried out in which the micrometeorological conditions have been studied over different small clearings plots of the forest. As these conditions can significantly affect many processes in the ecosystem, two questions arise: (1) whether and how the microclimatic conditions differ in the clear-cut and the gap, and (2) how heterogeneous the distribution of these conditions is on these plots. The aim of this study was to determine the spatial variation of air temperature on the clear-cut and gap as well as to compare the distribution of thermal and humidity conditions in both areas. The research was carried out in central Poland on a clear-cut with a width of 60 m and on a gap of an ellipsoid shape (40 × 70 m). The measurements were carried out in two series: spring–summer, during the period when the height of the sun during the day conditioned the inflow of direct solar radiation to any surface (May–August 2006), and autumn, when direct radiation was limited by neighbouring stands (October–November 2006). Average values of air temperature on the gap in the spring–summer period differed in individual parts of 2.2 °C, while on the clear-cut by 1.0 °C. In the autumn, thermal diversity on both research plots was similar (average 0.8 °C). The thermal diversity within the research areas was particularly marked in the case of extreme air temperature values. We found the modest spatial diversification of humidity parameters: vapour pressure, relative humidity, and humidity deficit. The particularly large diversification of relativity humidity and vapour pressure deficit occurred during the spring–summer period in the context of heat waves. The least beneficial thermal and humidity conditions for growing plants occurred in the north-eastern (NE) parts of the clear-cut and gap, which is why it is necessary to take particular note of these locations when undertaking silviculture.


2008 ◽  
Vol 65 (2) ◽  
pp. 297-308 ◽  
Author(s):  
Cindy Chu ◽  
Nicholas E Jones ◽  
Nicholas E Mandrak ◽  
Andrew R Piggott ◽  
Charles K Minns

The availability of suitable thermal habitat for fishes in streams is influenced by several factors, including flow, channel morphology, riparian vegetation, and land use. This study examined the influence of air temperature and groundwater discharge, predictors of stream temperature, on the thermal diversity (cold-, cool-, and warm-water preferences) of stream fish communities in southern Ontario watersheds. Site-level fish sampling data were used to assess the thermal diversity of 43 quaternary watersheds using three metrics, the proportion of sites within a watershed having (i) cold-, (ii) cool-, and (iii) warm-water fishes. Our results indicated that 53.9% of the variances in cold-water and 54.1% of the variances in warm-water fish distributions within the watersheds could be attributed to groundwater discharge and air temperature variables. Climate change scenarios suggested that watersheds with high groundwater discharge and the associated thermal diversity of fishes within those watersheds are less sensitive to climate change than watersheds with low groundwater discharge. Conservation of groundwater resources will be required to lessen climate change impacts on the thermal habitat and thermal diversity of stream fishes in southern Ontario watersheds.


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