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The results for the second scenario include a breakdown of the contribution with respect to rooftop categorization (see the 'Assessment strategies for community-scale potential' section).
In the 'Integral equation for the effective energy potential' section, we construct the integral equation governing the EPP on which all the subsequent results of this paper focus.
As such, the remainder of this assessment continued with assumptions regarding the building rooftops in this community (see the 'Assessment strategies for community-scale potential' section).
The 'Assessment strategies for community-scale potential' section describes the combination of the data and results from modeling for the estimation of community-scale potential.
As described in the 'Assessment strategies for community-scale potential' section, the first scenario relied on the horizontal plane assumption which viewed all buildings as having horizontal rooftops and equated the available mounting area with that of each building's footprint.
In particular, we focus on the clay-rich sediment at the base of the sedimentary section of the Pacific Plate, which is a potential section to be the plate boundary fault confirmed by Expedition 343 (Chester et al. 2013).
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We created a list of around 40 potential sections we expected to find, generated directly from elements specified in E3.
To avoid this potential loophole, Section 4(a)(1) is not available to affiliates.
A general connection of that sort may have been what Descartes had in mind when he suggested that attention to clear and distinct ideas is a necessary condition for those ideas to realize their special epistemic potential (see Section 1.1).
Gr7 is a function of modal shift potential (see section 3.3) but also technical difficulty and respondents have suggested this measure to have average modal shift potential and an above average difficulty rating.
Then, by applying Lemma 3.3 (where the time variable t coincides with the variable T in Eq. (28)) and assuming that the potential U (Section 3.2) is assigned as U ( y ) = φ 1 + y, we obtain the sought Eq. (18).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com