Accounting for Climate Change in Rainfall Intensity-Duration-Frequency (IDF) Curves for Stormwater Management by Christopher Martinez, Young Gu Her, Eban Bean

“… This publication is meant to describe three major approaches to account for climate change in rainfall intensity-duration-frequency (IDF) curves and the pros and cons of each approach. …”
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Rainfall Organization and Storm Tracking in Urban Barcelona, NE Spain, Using a High-Resolution Rain Gauge Network by María del Carmen Casas-Castillo, Xavier Navarro, Raül Rodríguez-Solà

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The Effect of Rainfall Patterns on the Mechanisms of Shallow Slope Failure by Muhammad Suradi, Andy Fourie

“…The results revealed that slopes are sensitive to rainfall pattern when the rainfall intensity has a high degree of fluctuation at around the same value as that of saturated hydraulic conductivity. …”
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Mangrove Landscaping As An Adaptation Pattern To Reduce The Impact of Climate Change in Segara Anakan Lagoon, Cilacap Regency Indonesia by Endang Hilmi, Nurul Anwar, Imam Santosa, Arif Mahdiana, Taruna Mona Rachman, Teguh Wardoyo

“…Climate change give a high impact on mangrove degradation (degradation 142.1 ha/year), the instability of rainfall intensity with average intensity 3552 mm/year, irregular wind direction with a speed average of 7 knots, and increasing of sea wave and sea level rise (range from 2.7 m to 3.4 m) The results conclude that the mangrove species have ability to live and grow, because the climate change does not affect mangrove growth (the correlation with rainfall intensity = -0,35, with wind speed = 0,18 and sea wave = - 0,34). …”
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Does rainfall create buoyant forcing at the ocean surface? by Dipanjan Chaudhuri, Eric A. D’Asaro

“…Furthermore, buoyancy fluxes during rain tend to be more positive at night than during the day, with nighttime rain twice as likely to cause instability compared to daytime rain, even at the same rainfall intensity. Average buoyancy fluxes across the tropics during rain can have either sign. …”
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Effect of nonwoven filters on rainfall seepage flow and stability of slopes by Koichi Tsubogo, Kohei Araki, Yasushi Fukuda, Keiji Kuwajima, Kosuke Katayama, Shunji Ue

“…In this paper, nonwoven filters were installed on the slope of an on-site observation area in the sediment disaster warning area north of National Institute of Technology, Tokuyama College in Shunan City, Yamaguchi Prefecture. The rainfall intensity and moisture content by volume were then measured in both the nonwoven filter installed and bare ground sections. …”
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The effects of climate change and flooding on the quality of education for secondary school students in Colombia by Martha Yánez Contreras, Boris Johnson Restrepo, Karina Acevedo González

“…To address potential bias related to the non-random distribution of floods, the study used a two-stage regression model with instrumental variables, incorporating indicators of rainfall intensity and geographical water coverage as instruments. …”
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ANALYSIS OF DELAY FACTORS IN THE CONSTRUCTION PROJECT OF THE PROMOTION CENTER BUILDING AND BATIK DERIVATIVE PRODUCTION BUILDING IN PAMEKASAN by Ahmad Fatoni, Fairus Zabadi, Muhammad Saifuddin

“…The most dominant causal factors are factors caused by external factors, namely in the form of very high rainfall intensity in one month and unilateral blockades by village officials. …”
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Spatial Variability and Time Stability of Throughfall in a Moso Bamboo (<i>Phyllostachys edulis</i>) Forest in Jinyun Mountain, China by Chunxia Liu, Yunqi Wang, Quanli Zong, Kai Jin, Peng Qin, Xiuzhi Zhu, Yujie Han

“…Throughfall CV had a significantly negative correlation with rainfall amount and rainfall intensity, whereas it increased with the increase in LAI. …”
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Identification and classification method of landslide pattern in the soil water index-based early warning system by Yulong Zhu, Bonan Wang, Yafen Zhang, Zhiguo Sun

“…Results indicate that the SWI-based EWS can identify and classify the four landslide patterns. As rainfall intensity rises, the slope failure pattern gradually changes from Pattern I (Sliding) during long-term low-intensity (LL) type rainfall, to Pattern II (Buckling), to Pattern III (Toppling), and finally to Pattern IV (Crumbling) during short-term high-intensity (SH) type rainfall. …”
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When and where does near-surface runoff occur in a pre-Alpine headwater catchment? by V. A. Gauthier, A. Leuteritz, I. van Meerveld

“…They increased with increasing precipitation and antecedent-wetness conditions but were not correlated with the rainfall intensity. Runoff ratios for OF were larger than 1 for some plots, indicating the occurrence of return flow from outside the plot. …”
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The Potential Use of the SCS-CN Method to Estimate Extreme Floods in the West Bank Data-scarce Catchments by Sameer Shadeed

“…This can be attributed to the expansion of urban areas together with the climate change impacts (the increasing rainfall intensity). This situation worsens given the lack of proper hydraulic infrastructures required to safely dispose of the accumulated floods. …”
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Assessment of soil infiltration capacity by using portable rainfall simulator by Yu. P. Sukhanovskii, V. A. Vitovtov, A. V. Prushchik, Yu. A. Solov`eva, S. I. Sanzharova

“…For both rainfall simulators the raindrops were of the same size, they fell down from the same height, the rainfall intensity was constant, but the values of these parameters seemed to be different. …”
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A Sub-Hourly Precipitation Dataset from a Pluviographic Network in Central Chile by Claudia Sangüesa, Alfredo Ibañez, Roberto Pizarro, Cristian Vidal-Silva, Pablo Garcia-Chevesich, Romina Mendoza, Cristóbal Toledo, Juan Pino, Rodrigo Paredes, Ben Ingram

“…This high temporal resolution is unprecedented for the region and enables detailed analysis of rainfall intensity, duration, and frequency patterns critical for hydrological research, climate studies, and water resource management in general. …”
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Summer soil moisture-convective precipitation coupling in Northern China at different timescales by Hongwei Yang, Zesu Yang, Hang He

“…The focus is on the influence of soil moisture on sensible and latent heat fluxes, which regulate the lifting condensation level (LCL) and boundary layer height (BLH).The results show a generally positive coupling between soil moisture and rainfall intensity in Northern China. Soil moisture and precipitation were generally positively correlated, with little variation in the area of positive coupling on the monthly and annual scales, which were both larger than on the daily scale, but were strongest on the annual scale in terms of coupling strength. …”
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Assessing the impact of climate change on flood patterns in downstream Nigeria using machine learning and geospatial techniques (2018–2024) by Desmond R. Eteh, Bunakiye R. Japheth, Charles U. Akajiaku, Ifunanya Osondu, Omabuwa O. Mene-Ejegi, Emmanuel M. Nwachukwu, Miebaka D. Oriasi, Erepamo J. Omietimi, Abiodun E. Ayo-Bali

“…Inundated areas increased from 20 to 35% of downstream zones. Rainfall intensity rose by 15–20%, with annual totals exceeding 4311 mm in some areas. …”
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Quantifying the impacts of diverse vegetation-covered patterns on hillslope soil erosion: a case experiment of alfalfa-covered hillslopes by Chong Yao, Qingwei Zhang, Kebing Chen, Shige Zhang, Ming Zhu, Zhijia Gu, Wei Yan, Faqi Wu

“…However, knowledge about the influence of herbage spatial distribution pattern on hillslope erosion is still limited.MethodsIn the current study, runoff plots (length × width × depth, 2 × 1 × 0.5 m) with slope gradient of 8.75%–36.40% and a side-spray rainfall simulator with rainfall intensity of 90 mm h-1 were adopted to rainfall simulation. …”
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Coastal Storm – Surge Combination Risk Identification and Resilience Planning Based on Supply and Demand Assessment of Flood Regulation Ecosystem Services: A Case Study of Fujian D... by Jian TIAN, Tianyu XIU, Suiping ZENG

“…Hazard indicators include rainfall intensity, and storm surge frequency and intensity, while vulnerability indicators encompass population density, economic development levels, and infrastructure fragility. …”
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Assessment of the Effect of Flooding on Agricultural Lands in Kaharo Sub-County of Kabale District South Western Uganda. by Nyakiti, Dorcas Awino

“…Rapid urbanization, population growth and high Rainfall Intensities were the causes of flooding on agricultural lands in Kaharo sub county Kabale district reported by 49%, 56% and 32%), respectively (Table 4.1). …”
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