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Water Cycle is an interdisciplinary open access journal that publishes top-tier original research in all areas of water cycles, including meta-cycles. It examines their relationship to science, technology, society, economics, health, culture, policy, regulation and strategy.
This paper presented a new optimization technique called the water cycle algorithm (WCA). The fundamental concepts and ideas which underlie the method are inspired from nature and based on the water cycle process in real world.
The terms ‘Grenvillian Orogeny’ (sensu lato) and ‘Grenville Orogenic Cycle’ are widely used in the geological literature to encompass the 1.3- to 1.0-Ga time-span of multiphase orogenic events.
For instance, abstract concepts, such as a desire to create a particular habitat feature, become linked to concrete imagery (King et al., 2021). Here we build on USACE guidance to show how innovative designs incorporating EWN concepts can enhance biodiversity associated with coastal projects.
Based on indicators of terrestrial water cycle intensity, this study evaluated changes in basin-scale hydrological cycle intensity from 1982 to 2017 and explored the large-scale circulation drivers behind it under climate change.
Research into the global water cycle mainly focus on: macroscopic characteristics of the water balance, energy balance and hydrothermal coupling balance at varying temporal and spatial scales; and the fluxes in the hydrological cycle occurring at the land-air interface (Brutsaert, 2005).
Moving toward a resilient urban water cycle has been identified as an opportunity to tackle urban water challenges by providing a systemic approach to delivering water supply and sanitation services in a more sustainable, inclusive, and efficient way (Howard et al., 2021; Liu et al., 2022).
Remnants of the Grenville Orogeny—a globally pervasive tectonothermal event resulting from the amalgamation of the supercontinent Rodinia between ca. 1.3 and 1.0 Ga—are exposed throughout eastern North America for ca. 3000 km from Labrador to Alabama.
To describe water flow into and out of a hydro-system (i.e., through the various hydrological processes) and quantify the rate of change in the water being stored in the hydro-system (i.e., in the land, atmosphere, and water bodies), a water balance equation is used.
Over the past few decades, the negative effects of climate extremities are reflected in hydrological cycle, viz., pronounced shifts in global precipitation patterns and increased atmospheric water vapor content, glacier melting, floods, soil erosion, and drought etc.