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Long-Term (1951–2007) Rainfall Trends around Six Indian Cities: Current State, Meteorological, and Urban Dynamics

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In this paper, the authors focused on analyzing the precipitation trends over six Indian cities during the summer monsoon (June-September) covering the period 1951-2007 and also attempted to investigate possible urban forcing and dynamics by examining the variation in precipitation in the upwind and downwind directions.

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Circulation background of climate patterns in the past millennium: Uncertainty analysis and re-reconstruction of ENSO-like state

TL;DR: Wang et al. as discussed by the authors integrated the Chinese stalagmite oxygen isotope sequence to reconstruct the tropical Pacific sea surface temperature gradient, i.e., the large-scale ENSO-like state over the past millennium.
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Spatial distribution of secular trends in rainfall indices of Peninsular Malaysia in the presence of long-term persistence

TL;DR: In this article, the authors assess the spatial patterns in the trends of annual and seasonal rainfall amounts and extremes in Peninsular Malaysia considering Long-Term Persistence (LTP) in hydroclimatic time series, which can lead to considerable change in the significance of trend.
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Spatiotemporal patterns and trends of Indian monsoonal rainfall extremes

TL;DR: This study provides a comprehensive analysis of trends in the extremes during the Indian summer monsoon months (June to September) at different temporal and spatial scales using quantile regression to identify and quantify spatiotemporal patterns and trends that have emerged during the recent decades and may be associated with changing climatic conditions.
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Spatial and seasonal variations of sand-dust events and their relation to atmospheric conditions and vegetation cover in semi-arid regions of central Iran

TL;DR: In this article, the authors used Ridge Regression (RR) method to analyze the relationship between seasonal variations of precipitation, surface winds speed, air temperature, and Enhanced Vegetation Index (EVI) with Dust Storm Index (DSI) for two different periods (2001-2008 and 2009-2016).
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Spatiotemporal trends in extreme rainfall and temperature indices over Upper Tapi Basin, India

TL;DR: In this paper, the long-term trends in extreme rainfall (1944-2013) and temperature (1969-2012) indices have been investigated at annual, seasonal, and monthly time scales using nonparametric Mann-Kendall (MK), modified MannK, and Sen's slope estimator tests.
References
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Proceedings ArticleDOI

A two-dimensional interpolation function for irregularly-spaced data

TL;DR: In many fields using empirical areal data there arises a need for interpolating from irregularly-spaced data to produce a continuous surface as discussed by the authors, and it is assumed that a unique number (such as rainfall in meteorology, or altitude in geography) is associated with each data point.
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Aerosols, climate, and the hydrological cycle

TL;DR: Human activities are releasing tiny particles (aerosols) into the atmosphere that enhance scattering and absorption of solar radiation, which can lead to a weaker hydrological cycle, which connects directly to availability and quality of fresh water, a major environmental issue of the 21st century.
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The Changing Character of Precipitation

TL;DR: In this article, precipitation intensity, duration, frequency, and phase are as much of concern as total amounts, as these factors determine the disposition of precipitation once it hits the ground and how much runs off.
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Global indirect aerosol effects: a review

TL;DR: In this article, the effects of aerosols on the climate system are discussed and different approaches how the climatic implications of these effects can be estimated globally as well as improvements that are needed in global climate models in order to better represent indirect aerosol effects are discussed.
Journal ArticleDOI

Constraints on future changes in climate and the hydrologic cycle

TL;DR: It will be substantially harder to quantify the range of possible changes in the hydrologic cycle than in global-mean temperature, both because the observations are less complete and because the physical constraints are weaker.
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