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Online Rainfall Atlas of Hawai‘i

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TLDR
The Rainfall Atlas of Hawai'i as discussed by the authors is a set of digitalmaps of the spatial patterns of the 1978-2007 meanmonthly and annual rainfall for the major Hawaiian islands.
Abstract
nteraction among trade winds,terrain, land thermal effects, andthe trade-wind inversion give theHawaiian Islands one of the mostvaried rainfall patterns on Earth.Distinct, persistent patterns of upliftlead to dramatic rainfall gradientsand, together with elevation-relatedtemperature differences, producenearly the full range of climate types.This microcosm of global environ-mental diversity provides a uniquenatural laboratory for world-classresearch on topics such as terres-trial ecosystem carbon dynamics, soilgeochemistry, and the mechanics ofspecies invasion. Knowledge of meanrainfall patterns in Hawai'i is criticallyimportant in support of these researchendeavors as well as for managing andprotecting groundwater and surfacewater resources, controlling and eradicating invasivespecies, protecting and restoring native ecosystems,and planning for the effects of global climate change.The Rainfall Atlas of Hawai'i is a set of digitalmaps of the spatial patterns of 1978-2007 meanmonthly and annual rainfall for the major Hawaiian

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WorldClim 2: new 1-km spatial resolution climate surfaces for global land areas

TL;DR: In this paper, the authors created a new dataset of spatially interpolated monthly climate data for global land areas at a very high spatial resolution (approximately 1 km2), including monthly temperature (minimum, maximum and average), precipitation, solar radiation, vapour pressure and wind speed, aggregated across a target temporal range of 1970-2000, using data from between 9000 and 60,000 weather stations.
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Climatologies at high resolution for the earth's land surface areas

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Our Skill in Modeling Mountain Rain and Snow is Bypassing the Skill of Our Observational Networks

TL;DR: In mountain terrain, well-configured high-resolution atmospheric models are able to simulate total annual rain and snowfall better than spatial estimates derived from in situ observational data as mentioned in this paper.
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Combining spectroscopic and isotopic techniques gives a dynamic view of phosphorus cycling in soil.

TL;DR: Spectroscopic and isotopic techniques are used to estimate turnover times of P pools and tease apart biologically-driven and geochemically-driven P fluxes, making possible a more dynamic, process-oriented conceptual model of P cycling in soils.
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Comparison of geostatistical approaches to spatially interpolate month-year rainfall for the Hawaiian Islands

TL;DR: In this article, three kriging algorithms, namely, Ordinary Kriging (OK), OCK and KED, were compared using cross-validation statistics, where OK produced the lowest error statistics.
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