Articles | Volume 24, issue 4
https://doi.org/10.5194/hess-24-1741-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-24-1741-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Apr 2020
Research article |
| 09 Apr 2020
| 09 Apr 2020
Near-0 °C surface temperature and precipitation type patterns across Canada
Meteorological Research Division, Environment and Climate Change
Canada, Toronto, M3H 5T4, Canada
Ronald E. Stewart
Department of Environment and Geography, University of Manitoba,
Winnipeg, R3T 2N2, Canada
Julie M. Theriault
Centre ESCER, Department of Earth and Atmospheric Sciences,
Université du Québec à Montréal, Montréal, H2X 3Y7, Canada
Bohdan Kochtubajda
Meteorological Service of Canada, Environment and Climate Change
Canada, Edmonton, T6B 1K5, Canada
Barrie R. Bonsal
Watershed Hydrology and Ecology Research Division, Environment and
Climate Change Canada, Saskatoon, S7N 3H5, Canada
Zhuo Liu
Department of Environment and Geography, University of Manitoba,
Winnipeg, R3T 2N2, Canada
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Matteo Colli, Mattia Stagnaro, Luca Lanza, Roy Rasmussen, and Julie M. Thériault
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Zhenhua Li, Yanping Li, Barrie Bonsal, Alan H. Manson, and Lucia Scaff
Hydrol. Earth Syst. Sci., 22, 5057–5067, https://doi.org/10.5194/hess-22-5057-2018, https://doi.org/10.5194/hess-22-5057-2018, 2018
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Julie M. Thériault, Ida Hung, Paul Vaquer, Ronald E. Stewart, and John W. Pomeroy
Hydrol. Earth Syst. Sci., 22, 4491–4512, https://doi.org/10.5194/hess-22-4491-2018, https://doi.org/10.5194/hess-22-4491-2018, 2018
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Precipitation events associated with rain and snow on the eastern slopes of the Rocky Mountains, Canada, are a critical aspect of the regional water cycle. The goal is to characterize the precipitation and weather conditions in the Kananaskis Valley, Alberta, during a field experiment. Mainly dense solid precipitation reached the surface and occurred during downslope and upslope conditions. The precipitation phase has critical implications on the severity of flooding events in the area.
Zilefac Elvis Asong, Howard Simon Wheater, Barrie Bonsal, Saman Razavi, and Sopan Kurkute
Hydrol. Earth Syst. Sci., 22, 3105–3124, https://doi.org/10.5194/hess-22-3105-2018, https://doi.org/10.5194/hess-22-3105-2018, 2018
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Canada is very susceptible to recurrent droughts, which have damaging impacts on regional water resources and agriculture. However, nationwide drought assessments are currently lacking and impacted by limited ground-based observations. We delineate two major drought regions (Prairies and northern central) over Canada and link drought characteristics to external factors of climate variability. This study helps to determine when the drought events occur, their duration, and how often they occur.
John Kochendorfer, Rodica Nitu, Mareile Wolff, Eva Mekis, Roy Rasmussen, Bruce Baker, Michael E. Earle, Audrey Reverdin, Kai Wong, Craig D. Smith, Daqing Yang, Yves-Alain Roulet, Tilden Meyers, Samuel Buisan, Ketil Isaksen, Ragnar Brækkan, Scott Landolt, and Al Jachcik
Hydrol. Earth Syst. Sci., 22, 1437–1452, https://doi.org/10.5194/hess-22-1437-2018, https://doi.org/10.5194/hess-22-1437-2018, 2018
Short summary
Short summary
Due to the effects of wind, precipitation gauges typically underestimate the amount of precipitation that occurs as snow. Measurements recorded during a World Meteorological Organization intercomparison of precipitation gauges were used to evaluate and improve the adjustments that are available to address this issue. Adjustments for specific types of precipitation gauges and wind shields were tested and recommended.
John Kochendorfer, Rodica Nitu, Mareile Wolff, Eva Mekis, Roy Rasmussen, Bruce Baker, Michael E. Earle, Audrey Reverdin, Kai Wong, Craig D. Smith, Daqing Yang, Yves-Alain Roulet, Samuel Buisan, Timo Laine, Gyuwon Lee, Jose Luis C. Aceituno, Javier Alastrué, Ketil Isaksen, Tilden Meyers, Ragnar Brækkan, Scott Landolt, Al Jachcik, and Antti Poikonen
Hydrol. Earth Syst. Sci., 21, 3525–3542, https://doi.org/10.5194/hess-21-3525-2017, https://doi.org/10.5194/hess-21-3525-2017, 2017
Short summary
Short summary
Precipitation measurements were combined from eight separate precipitation testbeds to create multi-site transfer functions for the correction of unshielded and single-Alter-shielded precipitation gauge measurements. Site-specific errors and more universally applicable corrections were created from these WMO-SPICE measurements. The importance and magnitude of such wind speed corrections were demonstrated.
Jefferson S. Wong, Saman Razavi, Barrie R. Bonsal, Howard S. Wheater, and Zilefac E. Asong
Hydrol. Earth Syst. Sci., 21, 2163–2185, https://doi.org/10.5194/hess-21-2163-2017, https://doi.org/10.5194/hess-21-2163-2017, 2017
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This study was conducted to quantify the spatial and temporal variability of the errors associated with various gridded precipitation products in Canada. Overall, WFDEI [GPCC] and CaPA performed best with respect to different performance measures, followed by ANUSPLIN and WEDEI [CRU]. Princeton and NARR demonstrated the lowest quality. Comparing the climate model-simulated products, PCIC ensembles generally performed better than NA-CORDEX ensembles in terms of reliability in four seasons.
L. Scaff, D. Yang, Y. Li, and E. Mekis
The Cryosphere, 9, 2417–2428, https://doi.org/10.5194/tc-9-2417-2015, https://doi.org/10.5194/tc-9-2417-2015, 2015
Short summary
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The bias corrections show significant errors in the gauge precipitation measurements over the northern regions. Monthly precipitation is closely correlated between the stations across the Alaska--Yukon border, particularly for the warm months. Double mass curves indicate changes in the cumulative precipitation due to bias corrections over the study period. Overall the bias corrections lead to a smaller and inverted precipitation gradient across the border, especially for snowfall.
Related subject area
Subject: Hydrometeorology | Techniques and Approaches: Mathematical applications
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Hydrol. Earth Syst. Sci., 28, 321–339, https://doi.org/10.5194/hess-28-321-2024, https://doi.org/10.5194/hess-28-321-2024, 2024
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Magdalena Uber, Michael Haller, Christoph Brendel, Gudrun Hillebrand, and Thomas Hoffmann
Hydrol. Earth Syst. Sci., 28, 87–102, https://doi.org/10.5194/hess-28-87-2024, https://doi.org/10.5194/hess-28-87-2024, 2024
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Yuanyuan Xiao, Shuiqing Yin, Bofu Yu, Conghui Fan, Wenting Wang, and Yun Xie
Hydrol. Earth Syst. Sci., 27, 4563–4577, https://doi.org/10.5194/hess-27-4563-2023, https://doi.org/10.5194/hess-27-4563-2023, 2023
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An exceptionally heavy rainfall event occurred on 20 July 2021 in central China (the 7.20 storm). The storm presents a rare opportunity to examine the extreme rainfall erosivity. The storm, with an average recurrence interval of at least 10 000 years, was the largest in terms of its rainfall erosivity on record over the past 70 years in China. The study suggests that extreme erosive events can occur anywhere in eastern China and are not necessarily concentrated in low latitudes.
Sara M. Vallejo-Bernal, Frederik Wolf, Niklas Boers, Dominik Traxl, Norbert Marwan, and Jürgen Kurths
Hydrol. Earth Syst. Sci., 27, 2645–2660, https://doi.org/10.5194/hess-27-2645-2023, https://doi.org/10.5194/hess-27-2645-2023, 2023
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Employing event synchronization and complex networks analysis, we reveal a cascade of heavy rainfall events, related to intense atmospheric rivers (ARs): heavy precipitation events (HPEs) in western North America (NA) that occur in the aftermath of land-falling ARs are synchronized with HPEs in central and eastern Canada with a delay of up to 12 d. Understanding the effects of ARs in the rainfall over NA will lead to better anticipating the evolution of the climate dynamics in the region.
Jiqing Li, Jing Huang, Lei Zheng, and Wei Zheng
Hydrol. Earth Syst. Sci., 27, 2325–2339, https://doi.org/10.5194/hess-27-2325-2023, https://doi.org/10.5194/hess-27-2325-2023, 2023
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Nele Reyniers, Timothy J. Osborn, Nans Addor, and Geoff Darch
Hydrol. Earth Syst. Sci., 27, 1151–1171, https://doi.org/10.5194/hess-27-1151-2023, https://doi.org/10.5194/hess-27-1151-2023, 2023
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Dipanjan Dey, Aitor Aldama Campino, and Kristofer Döös
Hydrol. Earth Syst. Sci., 27, 481–493, https://doi.org/10.5194/hess-27-481-2023, https://doi.org/10.5194/hess-27-481-2023, 2023
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One of the most striking and robust features of climate change is the acceleration of the atmospheric water cycle branch. Earlier studies were able to provide a quantification of the global atmospheric water cycle, but they missed addressing the atmospheric water transport connectivity within and between ocean basins and land. These shortcomings were overcome in the present study and presented a complete synthesised and quantitative view of the atmospheric water cycle.
Abbas El Hachem, Jochen Seidel, Florian Imbery, Thomas Junghänel, and András Bárdossy
Hydrol. Earth Syst. Sci., 26, 6137–6146, https://doi.org/10.5194/hess-26-6137-2022, https://doi.org/10.5194/hess-26-6137-2022, 2022
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Through this work, a methodology to identify outliers in intense precipitation data was presented. The results show the presence of several suspicious observations that strongly differ from their surroundings. Many identified outliers did not have unusually high values but disagreed with their neighboring values at the corresponding time steps. Weather radar and discharge data were used to distinguish between single events and false observations.
Qihua Ran, Jin Wang, Xiuxiu Chen, Lin Liu, Jiyu Li, and Sheng Ye
Hydrol. Earth Syst. Sci., 26, 4919–4931, https://doi.org/10.5194/hess-26-4919-2022, https://doi.org/10.5194/hess-26-4919-2022, 2022
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This study aims to further evaluate the relative importance of antecedent soil moisture and rainfall on flood generation and the controlling factors. The relative importance of antecedent soil moisture and daily rainfall present a significant correlation with drainage area; the larger the watershed, and the more essential the antecedent soil saturation rate is in flood generation, the less important daily rainfall will be.
Kyunghun Kim, Jaewon Jung, Hung Soo Kim, Masahiko Haraguchi, and Soojun Kim
Hydrol. Earth Syst. Sci., 26, 4823–4836, https://doi.org/10.5194/hess-26-4823-2022, https://doi.org/10.5194/hess-26-4823-2022, 2022
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This study applied a new methodology (complex network), instead of using classic methods, to establish the relationships between rainfall events in large East Asian cities. The relationships show that western China and Southeast Asia have a lot of influence on each other. Moreover, it is confirmed that the relationships arise from the effect of the East Asian monsoon. In future, complex network may be able to be applied to analyze the concurrent relationships between extreme rainfall events.
Haijiang Wu, Xiaoling Su, Vijay P. Singh, Te Zhang, Jixia Qi, and Shengzhi Huang
Hydrol. Earth Syst. Sci., 26, 3847–3861, https://doi.org/10.5194/hess-26-3847-2022, https://doi.org/10.5194/hess-26-3847-2022, 2022
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Agricultural drought forecasting lies at the core of overall drought risk management and is critical for food security and drought early warning. Using three-dimensional scenarios, we attempted to compare the agricultural drought forecast performance of a canonical vine copula (3C-vine) model and meta-Gaussian (MG) model over China. The findings show that the 3C-vine model exhibits more skill than the MG model when using 1– to 3-month lead times for forecasting agricultural drought.
Linqi Zhang, Yi Liu, Liliang Ren, Adriaan J. Teuling, Ye Zhu, Linyong Wei, Linyan Zhang, Shanhu Jiang, Xiaoli Yang, Xiuqin Fang, and Hang Yin
Hydrol. Earth Syst. Sci., 26, 3241–3261, https://doi.org/10.5194/hess-26-3241-2022, https://doi.org/10.5194/hess-26-3241-2022, 2022
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In this study, three machine learning methods displayed a good detection capacity of flash droughts. The RF model was recommended to estimate the depletion rate of soil moisture and simulate flash drought by considering the multiple meteorological variable anomalies in the adjacent time to drought onset. The anomalies of precipitation and potential evapotranspiration exhibited a stronger synergistic but asymmetrical effect on flash droughts compared to slowly developing droughts.
Abubakar Haruna, Juliette Blanchet, and Anne-Catherine Favre
Hydrol. Earth Syst. Sci., 26, 2797–2811, https://doi.org/10.5194/hess-26-2797-2022, https://doi.org/10.5194/hess-26-2797-2022, 2022
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Reliable prediction of floods depends on the quality of the input data such as precipitation. However, estimation of precipitation from the local measurements is known to be difficult, especially for extremes. Regionalization improves the estimates by increasing the quantity of data available for estimation. Here, we compare three regionalization methods based on their robustness and reliability. We apply the comparison to a dense network of daily stations within and outside Switzerland.
András Bárdossy, Jochen Seidel, and Abbas El Hachem
Hydrol. Earth Syst. Sci., 25, 583–601, https://doi.org/10.5194/hess-25-583-2021, https://doi.org/10.5194/hess-25-583-2021, 2021
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In this study, the applicability of data from private weather stations (PWS) for precipitation interpolation was investigated. Due to unknown errors and biases in these observations, a two-step filter was developed that uses indicator correlations and event-based spatial precipitation patterns. The procedure was tested and cross validated for the state of Baden-Württemberg (Germany). The biggest improvement is achieved for the shortest time aggregations.
Sigrid J. Bakke, Monica Ionita, and Lena M. Tallaksen
Hydrol. Earth Syst. Sci., 24, 5621–5653, https://doi.org/10.5194/hess-24-5621-2020, https://doi.org/10.5194/hess-24-5621-2020, 2020
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This study provides an in-depth analysis of the 2018 northern European drought. Large parts of the region experienced 60-year record-breaking temperatures, linked to high-pressure systems and warm surrounding seas. Meteorological drought developed from May and, depending on local conditions, led to extreme low flows and groundwater drought in the following months. The 2018 event was unique in that it affected most of Fennoscandia as compared to previous droughts.
Bo Dan, Xiaogu Zheng, Guocan Wu, and Tao Li
Hydrol. Earth Syst. Sci., 24, 5187–5201, https://doi.org/10.5194/hess-24-5187-2020, https://doi.org/10.5194/hess-24-5187-2020, 2020
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Data assimilation is a procedure to generate an optimal combination of the state variable in geoscience, based on the model outputs and observations. The ensemble Kalman filter (EnKF) scheme is a widely used assimilation method in soil moisture estimation. This study proposed several modifications of EnKF for improving this assimilation. The study shows that the quality of the assimilation result is improved, while the degree of water budget imbalance is reduced.
Eric Pohl, Christophe Grenier, Mathieu Vrac, and Masa Kageyama
Hydrol. Earth Syst. Sci., 24, 2817–2839, https://doi.org/10.5194/hess-24-2817-2020, https://doi.org/10.5194/hess-24-2817-2020, 2020
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Existing approaches to quantify the emergence of climate change require several user choices that make these approaches less objective. We present an approach that uses a minimum number of choices and showcase its application in the extremely sensitive, permafrost-dominated region of eastern Siberia. Designed as a Python toolbox, it allows for incorporating climate model, reanalysis, and in situ data to make use of numerous existing data sources and reduce uncertainties in obtained estimates.
Jianjun Zhang, Guangyao Gao, Bojie Fu, Cong Wang, Hoshin V. Gupta, Xiaoping Zhang, and Rui Li
Hydrol. Earth Syst. Sci., 24, 809–826, https://doi.org/10.5194/hess-24-809-2020, https://doi.org/10.5194/hess-24-809-2020, 2020
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We proposed an approach that integrates universal multifractals and a segmentation algorithm to precisely identify extreme precipitation (EP) and assess spatiotemporal EP variation over the Loess Plateau, using daily data. Our results explain how EP contributes to the widely distributed severe natural hazards. These findings are of great significance for ecological management in the Loess Plateau. Our approach is also helpful for spatiotemporal EP assessment at the regional scale.
Tongtiegang Zhao, Wei Zhang, Yongyong Zhang, Zhiyong Liu, and Xiaohong Chen
Hydrol. Earth Syst. Sci., 24, 1–16, https://doi.org/10.5194/hess-24-1-2020, https://doi.org/10.5194/hess-24-1-2020, 2020
Guoxiao Wei, Xiaoying Zhang, Ming Ye, Ning Yue, and Fei Kan
Hydrol. Earth Syst. Sci., 23, 2877–2895, https://doi.org/10.5194/hess-23-2877-2019, https://doi.org/10.5194/hess-23-2877-2019, 2019
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Accurately evaluating evapotranspiration (ET) is a critical challenge in improving hydrological process modeling. Here we evaluated four ET models (PM, SW, PT–FC, and AA) under the Bayesian framework. Our results reveal that the SW model has the best performance. This is in part because the SW model captures the main physical mechanism in ET; the other part is that the key parameters, such as the extinction factor, could be well constrained with observation data.
Chongli Di, Tiejun Wang, Xiaohua Yang, and Siliang Li
Hydrol. Earth Syst. Sci., 22, 5069–5079, https://doi.org/10.5194/hess-22-5069-2018, https://doi.org/10.5194/hess-22-5069-2018, 2018
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The original Grassberger–Procaccia algorithm for complex analysis was modified by incorporating the normal-based K-means clustering technique and the RANSAC algorithm. The calculation accuracy of the proposed method was shown to outperform traditional algorithms. The proposed algorithm was used to diagnose climate system complexity in the Hai He basin. The spatial patterns of the complexity of precipitation and air temperature reflected the influence of the dominant climate system.
César Cisneros Vaca, Christiaan van der Tol, and Chandra Prasad Ghimire
Hydrol. Earth Syst. Sci., 22, 3701–3719, https://doi.org/10.5194/hess-22-3701-2018, https://doi.org/10.5194/hess-22-3701-2018, 2018
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The influence of long-term changes in canopy structure on rainfall interception loss was studied in a 55-year old forest. Interception loss was similar at the same site (38 %), when the forest was 29 years old. In the past, the forest was denser and had a higher storage capacity, but the evaporation rates were lower. We emphasize the importance of quantifying downward sensible heat flux and heat release from canopy biomass in tall forest in order to improve the quantification of evaporation.
Sojung Park, Seon Ki Park, Jeung Whan Lee, and Yunho Park
Hydrol. Earth Syst. Sci., 22, 3435–3452, https://doi.org/10.5194/hess-22-3435-2018, https://doi.org/10.5194/hess-22-3435-2018, 2018
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Understanding the precipitation characteristics is essential to design an optimal observation network. We studied the spatial and temporal characteristics of summertime precipitation systems in Korea via geostatistical analyses on the ground-based precipitation and satellite water vapor data. We found that, under a strict standard, an observation network with higher resolution is required in local areas with frequent heavy rainfalls, depending on directional features of precipitation systems.
Wenbin Liu, Fubao Sun, Yanzhong Li, Guoqing Zhang, Yan-Fang Sang, Wee Ho Lim, Jiahong Liu, Hong Wang, and Peng Bai
Hydrol. Earth Syst. Sci., 22, 351–371, https://doi.org/10.5194/hess-22-351-2018, https://doi.org/10.5194/hess-22-351-2018, 2018
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The dynamics of basin-scale water budgets over the Tibetan Plateau (TP) are not well understood nowadays due to the lack of hydro-climatic observations. In this study, we investigate seasonal cycles and trends of water budget components (e.g. precipitation P, evapotranspiration ET and runoff Q) in 18 TP river basins during the period 1982–2011 through the use of multi-source datasets (e.g. in situ observations, satellite retrievals, reanalysis outputs and land surface model simulations).
Harsh Beria, Trushnamayee Nanda, Deepak Singh Bisht, and Chandranath Chatterjee
Hydrol. Earth Syst. Sci., 21, 6117–6134, https://doi.org/10.5194/hess-21-6117-2017, https://doi.org/10.5194/hess-21-6117-2017, 2017
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High-quality satellite precipitation forcings have provided a viable alternative to hydrologic modeling in data-scarce regions. Ageing TRMM sensors have recently been upgraded to GPM, promising enhanced spatio-temporal resolutions. Statistical and hydrologic evaluation of GPM measurements across 86 Indian river basins revealed improved low rainfall estimates with reduced effects of climatology and topography.
James C. Bennett, Quan J. Wang, David E. Robertson, Andrew Schepen, Ming Li, and Kelvin Michael
Hydrol. Earth Syst. Sci., 21, 6007–6030, https://doi.org/10.5194/hess-21-6007-2017, https://doi.org/10.5194/hess-21-6007-2017, 2017
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We assess a new streamflow forecasting system in Australia. The system is designed to meet the need of water agencies for 12-month forecasts. The forecasts perform well in a wide range of rivers. Forecasts for shorter periods (up to 6 months) are generally informative. Forecasts sometimes did not perform well in a few very dry rivers. We test several techniques for improving streamflow forecasts in drylands, with mixed success.
Konrad Bogner, Katharina Liechti, and Massimiliano Zappa
Hydrol. Earth Syst. Sci., 21, 5493–5502, https://doi.org/10.5194/hess-21-5493-2017, https://doi.org/10.5194/hess-21-5493-2017, 2017
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The enhanced availability of many different weather prediction systems nowadays makes it very difficult for flood and water resource managers to choose the most reliable and accurate forecast. In order to circumvent this problem of choice, different approaches for combining this information have been applied at the Sihl River (CH) and the results have been verified. The outcome of this study highlights the importance of forecast combination in order to improve the quality of forecast systems.
Matthew B. Switanek, Peter A. Troch, Christopher L. Castro, Armin Leuprecht, Hsin-I Chang, Rajarshi Mukherjee, and Eleonora M. C. Demaria
Hydrol. Earth Syst. Sci., 21, 2649–2666, https://doi.org/10.5194/hess-21-2649-2017, https://doi.org/10.5194/hess-21-2649-2017, 2017
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The commonly used bias correction method called quantile mapping assumes a constant function of error correction values between modeled and observed distributions. Our article finds that this function cannot be assumed to be constant. We propose a new bias correction method, called scaled distribution mapping, that does not rely on this assumption. Furthermore, the proposed method more explicitly accounts for the frequency of rain days and the likelihood of individual events.
Tesfay G. Gebremicael, Yasir A. Mohamed, Pieter v. Zaag, and Eyasu Y. Hagos
Hydrol. Earth Syst. Sci., 21, 2127–2142, https://doi.org/10.5194/hess-21-2127-2017, https://doi.org/10.5194/hess-21-2127-2017, 2017
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This study was conducted to understand the spatio-temporal variations of streamflow in the Tekezē basin. Results showed rainfall over the basin did not significantly change. However, streamflow experienced high variabilities at seasonal and annual scales. Further studies are needed to verify hydrological changes by identifying the physical mechanisms behind those changes. Findings are useful as prerequisite for studying the effects of catchment management dynamics on the hydrological processes.
Louise Crochemore, Maria-Helena Ramos, Florian Pappenberger, and Charles Perrin
Hydrol. Earth Syst. Sci., 21, 1573–1591, https://doi.org/10.5194/hess-21-1573-2017, https://doi.org/10.5194/hess-21-1573-2017, 2017
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The use of general circulation model outputs for streamflow forecasting has developed in the last decade. In parallel, traditional streamflow forecasting is commonly based on historical data. This study investigates the impact of conditioning historical data based on circulation model precipitation forecasts on seasonal streamflow forecast quality. Results highlighted a trade-off between the sharpness and reliability of forecasts.
Louise Crochemore, Maria-Helena Ramos, and Florian Pappenberger
Hydrol. Earth Syst. Sci., 20, 3601–3618, https://doi.org/10.5194/hess-20-3601-2016, https://doi.org/10.5194/hess-20-3601-2016, 2016
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This study investigates the way bias correcting precipitation forecasts can improve the skill of streamflow forecasts at extended lead times. Eight variants of bias correction approaches based on the linear scaling and the distribution mapping methods are applied to the precipitation forecasts prior to generating the streamflow forecasts. One of the main results of the study is that distribution mapping of daily values is successful in improving forecast reliability.
P. Froidevaux, J. Schwanbeck, R. Weingartner, C. Chevalier, and O. Martius
Hydrol. Earth Syst. Sci., 19, 3903–3924, https://doi.org/10.5194/hess-19-3903-2015, https://doi.org/10.5194/hess-19-3903-2015, 2015
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We investigate precipitation characteristics prior to 4000 annual floods in Switzerland since 1961. The floods were preceded by heavy precipitation, but in most catchments extreme precipitation occurred only during the last 3 days prior to the flood events. Precipitation sums for earlier time periods (like e.g. 4-14 days prior to floods) were mostly average and do not correlate with the return period of the floods.
G. H. Fang, J. Yang, Y. N. Chen, and C. Zammit
Hydrol. Earth Syst. Sci., 19, 2547–2559, https://doi.org/10.5194/hess-19-2547-2015, https://doi.org/10.5194/hess-19-2547-2015, 2015
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This study compares the effects of five precipitation and three temperature correction methods on precipitation, temperature, and streamflow through loosely coupling RCM (RegCM) and a distributed hydrological model (SWAT) in terms of frequency-based indices and time-series-based indices. The methodology and results can be used for other regions and other RCM and hydrologic models, and for impact studies of climate change on water resources at a regional scale.
M. S. Siam and E. A. B. Eltahir
Hydrol. Earth Syst. Sci., 19, 1181–1192, https://doi.org/10.5194/hess-19-1181-2015, https://doi.org/10.5194/hess-19-1181-2015, 2015
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This paper explains the different natural modes of interannual variability in the flow of the Nile River and also presents a new index based on the sea surface temperature (SST) over the southern Indian Ocean to forecast the flow of the Nile River. It also presents a new hybrid forecasting algorithm that can be used to predict the Nile flow based on indices of the SST in the eastern Pacific and southern Indian oceans.
D. Halwatura, A. M. Lechner, and S. Arnold
Hydrol. Earth Syst. Sci., 19, 1069–1091, https://doi.org/10.5194/hess-19-1069-2015, https://doi.org/10.5194/hess-19-1069-2015, 2015
G. Panthou, T. Vischel, T. Lebel, G. Quantin, and G. Molinié
Hydrol. Earth Syst. Sci., 18, 5093–5107, https://doi.org/10.5194/hess-18-5093-2014, https://doi.org/10.5194/hess-18-5093-2014, 2014
D. Masson and C. Frei
Hydrol. Earth Syst. Sci., 18, 4543–4563, https://doi.org/10.5194/hess-18-4543-2014, https://doi.org/10.5194/hess-18-4543-2014, 2014
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The question of how to utilize information from the physiography/topography in the spatial interpolation of rainfall is a long-standing discussion in the literature. In this study we test ideas that go beyond the approach in popular interpolation schemes today. The key message of our study is that these ideas can at best marginally improve interpolation accuracy, even in a region where a clear benefit would intuitively be expected.
A. Casanueva, C. Rodríguez-Puebla, M. D. Frías, and N. González-Reviriego
Hydrol. Earth Syst. Sci., 18, 709–725, https://doi.org/10.5194/hess-18-709-2014, https://doi.org/10.5194/hess-18-709-2014, 2014
D. H. Yan, D. Wu, R. Huang, L. N. Wang, and G. Y. Yang
Hydrol. Earth Syst. Sci., 17, 2859–2871, https://doi.org/10.5194/hess-17-2859-2013, https://doi.org/10.5194/hess-17-2859-2013, 2013
F. Yusof, I. L. Kane, and Z. Yusop
Hydrol. Earth Syst. Sci., 17, 1311–1318, https://doi.org/10.5194/hess-17-1311-2013, https://doi.org/10.5194/hess-17-1311-2013, 2013
J. H. Lee, J. Timmermans, Z. Su, and M. Mancini
Hydrol. Earth Syst. Sci., 16, 4291–4302, https://doi.org/10.5194/hess-16-4291-2012, https://doi.org/10.5194/hess-16-4291-2012, 2012
L. Gudmundsson, J. B. Bremnes, J. E. Haugen, and T. Engen-Skaugen
Hydrol. Earth Syst. Sci., 16, 3383–3390, https://doi.org/10.5194/hess-16-3383-2012, https://doi.org/10.5194/hess-16-3383-2012, 2012
T. Bosshard, S. Kotlarski, T. Ewen, and C. Schär
Hydrol. Earth Syst. Sci., 15, 2777–2788, https://doi.org/10.5194/hess-15-2777-2011, https://doi.org/10.5194/hess-15-2777-2011, 2011
S. Nie, J. Zhu, and Y. Luo
Hydrol. Earth Syst. Sci., 15, 2437–2457, https://doi.org/10.5194/hess-15-2437-2011, https://doi.org/10.5194/hess-15-2437-2011, 2011
G. Ibarra-Berastegi, J. Saénz, A. Ezcurra, A. Elías, J. Diaz Argandoña, and I. Errasti
Hydrol. Earth Syst. Sci., 15, 1895–1907, https://doi.org/10.5194/hess-15-1895-2011, https://doi.org/10.5194/hess-15-1895-2011, 2011
R. Schiemann, R. Erdin, M. Willi, C. Frei, M. Berenguer, and D. Sempere-Torres
Hydrol. Earth Syst. Sci., 15, 1515–1536, https://doi.org/10.5194/hess-15-1515-2011, https://doi.org/10.5194/hess-15-1515-2011, 2011
A. Lü, S. Jia, W. Zhu, H. Yan, S. Duan, and Z. Yao
Hydrol. Earth Syst. Sci., 15, 1273–1281, https://doi.org/10.5194/hess-15-1273-2011, https://doi.org/10.5194/hess-15-1273-2011, 2011
G. Wang, A. J. Dolman, and A. Alessandri
Hydrol. Earth Syst. Sci., 15, 57–64, https://doi.org/10.5194/hess-15-57-2011, https://doi.org/10.5194/hess-15-57-2011, 2011
F. Garavaglia, J. Gailhard, E. Paquet, M. Lang, R. Garçon, and P. Bernardara
Hydrol. Earth Syst. Sci., 14, 951–964, https://doi.org/10.5194/hess-14-951-2010, https://doi.org/10.5194/hess-14-951-2010, 2010
Cited articles
Ahrens, C. D., Jackson, P. L., and Jackson, C. E. J.: Meteorology Today: An
introduction to weather, climate, and the environment, Second Canadian
edition, Nelson Education, ISBN-13: 978-0176530792, 2015.
American Meteorological Society: Chinook, Glossary of Meteorology, available at: http://glossary.ametsoc.org/wiki/Chinook (last access date: 2 April 2020), 2012.
American Meteorological Society: Glossary of Meteorology, available at:
http://glossary.ametsoc.org/wiki/Main_Page (last access:
3 October 2019), 2018.
Auer Jr., A. H.: The rain versus snow threshold temperatures, Weatherwise,
27, 67–67, 1974.
Beltaos, S., Prowse, T., Bonsal, B., Mackay, R., Romolo, L., Pietroniro, A.,
and Toth, B.: Climatic effects on ice-jam flooding of the Peace-Athabasca
Delta, Hydrol. Process., 20, 4031–4050, https://doi.org/10.1002/hyp.6418,
2006.
Bonsal, B. R. and Prowse, T. D.: Trends and variability in spring and autumn
0 ∘C-isotherm dates over Canada, Climatic Change, 57, 341–358,
https://doi.org/10.1023/a:1022810531237, 2003.
Boone, A., Masson, V., Meyers, T., and Noilhan, J.: The influence of the
inclusion of soil freezing on simulations by a soil–vegetation–atmosphere
transfer scheme, J. Appl. Meteorol., 39, 1544–1569, https://doi.org/10.1175/1520-0450(2000)039<1544:TIOTIO>2.0.CO;2, 2000.
Bresson, É., Laprise, R., Paquin, D., Thériault, J., and Elía,
R. D.: Evaluating the ability of CRCM5 to simulate mixed precipitation,
Atmos.-Ocean, 55, 79–93, https://doi.org/10.1080/07055900.2017.1310084, 2017.
Brinkmann, W. and Ashwell, I.: The structure and movement of the chinook in
Alberta, Atmosphere, 6, 1–10, https://doi.org/10.1080/00046973.1968.9676548, 1968.
Bush, E. and Lemmen, D. S. (Eds.): Canada's changing climate report,
Government of Canada, Ottawa, Ontario, 444 pp., 2019.
Carrière, J.-M., Lainard, C., Bot, C. L., and Robart, F.: A
climatological study of surface freezing precipitation in Europe,
Meteorol. Appl., 7, 229–238, https://doi.org/10.1017/s1350482700001560,
2000.
Changnon, S. A.: Characteristics of ice storms in the United States, J.
Appl. Meteorol., 42, 630–639,
https://doi.org/10.1175/1520-0450(2003)042<0630:coisit>2.0.co;2,
2003.
Cortinas, J.: A climatology of freezing rain in the Great Lakes region of
North America, Mon. Weather Rev., 128, 3574–3588,
https://doi.org/10.1175/1520-0493(2001)129<3574:acofri>2.0.co;2,
2000.
Dai, A.: Temperature and pressure dependence of the rain-snow phase
transition over land and ocean, Geophys. Res. Lett., 35, L12802, https://doi.org/10.1029/2008GL033295, 2008.
ECCC (Environment and Climate Change Canada): Historical Climate Data
portal, available at: http://www.climate.weatheroffice.ec.gc.ca, last
access: 3 October 2019a.
ECCC (Environment and Climate Change Canada): MANOBS (Manual of Surface
Weather Observation Standards), 8th Edition, available at:
https://www.canada.ca/en/environment-climate-change/services/weather-manuals-documentation/manobs-surface-observations.html,
last access: 3 October 2019b.
ECCC (Environment and Climate Change Canada): Canadian Climate Normals,
available at: http://climate.weather.gc.ca/climate_normals/index_e.html, last access: 24 October 2019c.
Frei, C. and Schär, C.: Detection probability of trends in rare
events: Theory and application to heavy precipitation in the Alpine region,
J. Climate, 14, 1568–1584, 2001.
Fujibe, F.: On the near-0 ∘C. frequency maximum in surface air
temperature under precipitation: A statistical evidence for the melting
effect, J. Meteorol. Soc. Jpn., 79, 731–739,
2001.
Groenemeijer, P., Becker, N., Djidara, M., Gavin, K., Hellenberg, T.,
Holzer, A. M., Juga, I., Jokinen, P., Jylhä, K., Lehtonen, I.,
Mäkelä, H., Napoles, O., Nissen, K., Paprotny, D., Prak, P.,
Púčik, T., Tijssen L., and Vajda, A.: Past Cases of Extreme Weather
Impact on Critical Infrastructure in Europe. Office of Critical
Infrastructure Protection and Emergency Preparedness, FP7-SEC-2013-1, 129 pp., 2017.
Groisman, P. Y., Bulygina, O. N., Yin, X., Vose, R. S., Gulev, S. K.,
Hanssen-Bauer, I., and Førland, E.: Recent changes in the frequency of
freezing precipitation in North America and Northern Eurasia, Environ.
Res. Lett., 11, 045007, https://doi.org/10.1088/1748-9326/11/4/045007, 2016.
Gullett, D. W. and Skinner, W. R.: The state of Canada's climate: temperature change in Canada 1895-1991, SOE Report no. 92-2. Catalogue No. En 1-11/92-2E.A, State of the Environment Report, ISSN 0843-6193, Toronto, ON, Environment Canada, 1992.
Hare, K.: Canada's climate: An overall perspective, in: “The Surface
Climates of Canada”, McGill-Queen's University Press, 3–20, 1997.
Henson, W., Stewart, R., and Kochtubajda, B.: On the precipitation and
related features of the 1998 Ice Storm in the Montréal area, Atmos.
Res., 83, 36–54, https://doi.org/10.1016/j.atmosres.2006.03.006, 2007.
Henson, W., Stewart, R., Kochtubajda, B., and Thériault, J.: The 1998 Ice
Storm: Local flow fields and linkages to precipitation, Atmos.
Res., 101, 852–862, https://doi.org/10.1016/j.atmosres.2011.05.014, 2011.
Houston, T. G. and Changnon, S. A.: Freezing rain events: a major weather
hazard in the conterminous US, Nat. Hazards, 40, 485–494,
https://doi.org/10.1007/s11069-006-9006-0, 2007.
Intergovernmental Panel on Climate Change: Climate Change 2013: The Physical
Science Basis, Contribution of Working Group I to the Fifth Assessment
Report of the Intergovernmental Panel on Climate Change, edited by: Stocker, T. F.,
Qin, D., Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels,
A., Xia, Y., Bex, V., and Midgley, P. M., Cambridge University Press,
Cambridge, United Kingdom and New York, NY, USA, 1535 pp.,
https://doi.org/10.1017/CBO9781107415324, 2013.
Jennings, K. S., Winchell, T. S., Livneh, B., and Molotch, N. P.: Spatial
variation of the rain–snow temperature threshold across the Northern
Hemisphere, Nat. Commun., 9, 1148, https://doi.org/10.1038/s41467-018-03629-7,
2018.
Jeong, D. I., Cannon, A. J., and Zhang, X.: Projected changes to extreme freezing precipitation and design ice loads over North America based on a large ensemble of Canadian regional climate model simulations, Nat. Hazards Earth Syst. Sci., 19, 857–872, https://doi.org/10.5194/nhess-19-857-2019, 2019.
Kämäräinen, M., Hyvärinen, O., Jylhä, K., Vajda, A., Neiglick, S., Nuottokari, J., and Gregow, H.: A method to estimate freezing rain climatology from ERA-Interim reanalysis over Europe, Nat. Hazards Earth Syst. Sci., 17, 243–259, https://doi.org/10.5194/nhess-17-243-2017, 2017.
Keim, B. D. and Cruise, J. F.: A technique to measure trends in the
frequency of discrete random events, J. Climate, 11, 848–855, 1998.
Kendall, M. B.: Rank Correlation Methods, Hafner Publishing Company, New
York, 1955.
Kerry, M., Kelk, G., Etkin, D., Burton, I., and Kalhok, S.: Glazed over: Canada
copes with the Ice Storm of 1998, Environment, 41, 6–11, 1999.
Kienzle, S. W.: A new temperature based method to separate rain and snow,
Hydrol. Process., 22, 5067–5085, https://doi.org/10.1002/hyp.7131, 2008.
Klaassen, J., Cheng, C. S., Auld, H., Li, Q., Ros, E., Geast, M., Li, G., and
Lee, R.: Estimation of Severe Ice Storm Risks for South-Central Canada.
Report prepared for Office of Critical Infrastructure Protection and
Emergency Preparedness, Meteorological Service of Canada, Environment
Canada, Toronto, Canada, 2003.
Kochtubajda, B., Mooney, C., and Stewart, R.: Characteristics, atmospheric
drivers and occurrence patterns of freezing precipitation and ice pellets
over the Prairie Provinces and Arctic Territories of Canada: 1964–2005,
Atmos. Res., 191, 115–127, https://doi.org/10.1016/j.atmosres.2017.03.005,
2017.
Kraatz, S., Jacobs, J. M., and Miller, H. J.: Spatial and temporal
freeze-thaw variations in Alaskan roads, Cold Reg. Sci.
Technol., 157, 149–162, https://doi.org/10.1016/j.coldregions.2018.10.006, 2019.
Lambert, S. J. and Hansen, B. K.: Simulated changes in the freezing rain
Climatology of North America under global warming using a coupled climate
model, Atmos.-Ocean, 49, 289–295, https://doi.org/10.1080/07055900.2011.607492,
2011.
Larouche, P. and Galbraith, P. S.: Canadian coastal seas and Great Lakes Sea
Surface Temperature climatology and recent trends, Can. J.
Remote Sens., 42, 243–258, https://doi.org/10.1080/07038992.2016.1166041, 2016.
Laute, K. and Beylich, A. A.: Potential effects of climate change on future
snow avalanche activity in western Norway deduced from meteorological data,
Geogr. Ann. A, 100, 163–184,
https://doi.org/10.1080/04353676.2018.1425622, 2018.
Lecomte, E. L., Pang, A. W., and Russell, J. W.: Ice Storm '98. Institute for
Catastrophic Loss Reduction, Toronto, Ontario, Research Paper Series 1, 37 pp., 1998.
Lindenschmidt, K.-E., Das, A., Rokaya, P., and Chu, T.: Ice-jam flood risk
assessment and mapping, Hydrol. Process., 30, 3754–3769,
https://doi.org/10.1002/hyp.10853, 2016.
Longley, R. W.: The frequency of winter chinooks in Alberta, Atmosphere,
5, 4–16, https://doi.org/10.1080/00046973.1967.9676538, 1967.
MacKay, G. A. and Thompson, H. A.: Estimating the hazard of ice accretion in
Canada from climatological data, J. Appl. Meteorol., 8,
927–935, https://doi.org/10.1175/1520-0450(1969)008<0927:ethoia>2.0.co;2, 1969.
Matsuo, T. and Sasyo, Y.: Empirical formula for the melting rate of
snowflakes, J. Meteorol. Soc. Jpn. Ser. II, 59,
1–9, https://doi.org/10.2151/jmsj1965.59.1_1, 1981a.
Matsuo, T. and Sasyo, Y.: Melting of snowflakes below freezing level in the
atmosphere, J. Meteorol. Soc. Jpn. Ser. II, 59,
10–25, https://doi.org/10.2151/jmsj1965.59.1_10, 1981b.
Matsuo, T., Sasyo, Y., and Sato, Y.: Relationship between types of
precipitation on the ground and surface meteorological elements, J.
Meteorol. Soc. Jpn. Ser. II, 59, 462–476,
https://doi.org/10.2151/jmsj1965.59.4_462, 1981.
Matte, D., Thériault, J. M., and Laprise, R.: Mixed precipitation
occurrences over southern Québec, Canada, under warmer climate
conditions using a regional climate model, Clim. Dynam., 53, 1125–1141,
https://doi.org/10.1007/s00382-018-4231-2, 2019.
McCullagh, P. and Nelder, J. A.: Generalized linear models, 2nd ed.,
Monogr. on Statistics and Appl. Probability, No. 37, Chapman and Hall,
London, UK, 1989.
McFadden, V. and Thériault, J. M.: Simulations of the ice storm in
the Maritime Provinces on 24–26 January 2017, Canadian Meteorological and
Oceanographic Society Congress, Halifax, Nova Scotia, 2018.
McKenney, D. W., Pedlar, J. H., Lawrence, K., Papadopol, P., Campbell, K.,
and Hutchinson, M. F.: Change and evolution in the plant hardiness zones of
Canada, BioScience, 64, 341–350, https://doi.org/10.1093/biosci/biu016, 2014.
Mekis, É., Vincent, L. A., Shephard, M. W., and Zhang, X.: Observed trends in severe weather conditions based on humidex, wind chill, and heavy rainfall events in Canada for 1953–2012, Atmos.-Ocean, 53, 383–397, https://doi.org/10.1080/07055900.2015.1086970, 2015.
Mekis, E., Donaldson, N., Reid, J., Zucconi, A., Hoover, J., Li, Q., Nitu,
R., and Melo, S.: An overview of surface-based precipitation observations at
Environment and Climate Change Canada, Atmos.-Ocean, 56, 71–95,
https://doi.org/10.1080/07055900.2018.1433627, 2018.
Mendoza, G.-P. and Schmunk, R.: Fraser Valley ice storm creates slippery
roads, leaves thousands without power | CBC News, CBCnews, available at:
https://www.cbc.ca/news/canada/british-columbia/fraser-valley-winter-storm-december-2017-1.4467154 (last access: 2 April 2020),
2017.
Milton, J. and Bourque, A.: A climatological account of the January 1998 Ice
Storm in Québec, Atmospheric Sciences and Environmental Issues Division,
Environment Canada, Québec Region, 87 pp., 1999.
Moen, J. and Fredman, P.: Effects of climate change on alpine skiing in
Sweden, J. Sustain. Tour., 15, 418–437,
https://doi.org/10.2167/jost624.0, 2007.
Nitu, R., Roulet, Y. A., Wolff, M., Earle, M., Reverdin, A., Smith, C.,
Kochendorfer, J., Morin, S., Rasmussen, R., Wong, K., Alastrué, J.,
Arnold, L., Baker, B., Buisán, S., Collado, J. L., Colli, M., Collins,
B., Gaydos, A., Hannula, H. R., Hoover, J., Joe, P., Kontu, A., Laine, T.,
Lanza, L., Lanzinger, E., Lee, G. W., Lejeune, Y., Leppänen, L., Mekis,
E., Panel, J. M., Poikonen, A., Ryu, S., Sabatini, F., Theriault, J., Yang,
D., Genthon, C., van den Heuvel, F., Hirasawa, N., Konishi, H., Nishimura,
K., and Senese, A.: WMO Solid Precipitation Intercomparison Experiment
(SPICE) (2012–2015), World Meteorological Organization Instruments and
Observing Methods Report No. 131, Geneva, 2018.
Nkemdirim, L. C.: Canada's chinook belt, Int. J.
Climatol., 16, 441–462,
https://doi.org/10.1002/(sici)1097-0088(199604)16:4< 441::aid-joc21>3.0.co;2-t, 1996.
Phillips, D.: The Climates of Canada, Supply and Services Canada, Ottawa,
176 pp., 1990.
Sen, P. K.: Estimates of the regression coefficient Based on Kendall's tau,
J. Am. Stat. Assoc., 63, 1379–1389,
https://doi.org/10.1080/01621459.1968.10480934, 1968.
Sims, E. M. and Liu, G.: A parameterization of the probability of snow–rain
transition, J. Hydrometeorol., 16, 1466–1477,
https://doi.org/10.1175/jhm-d-14-0211.1, 2015.
Stewart, R. and Patenaude, L.: Rain-snow boundaries and freezing
precipitation in Canadian East Coast winter storms, Atmos.-Ocean, 26,
377–398, https://doi.org/10.1080/07055900.1988.9649309, 1988.
Stewart, R. E.: Precipitation types in winter storms, Pure Appl.
Geophys., 123, 597–609, 1985.
Stewart, R. E. and Yiu, D. T.: Distributions of precipitation and associated
parameters across precipitation type transitions over southern Ontario,
Atmos. Res., 29, 153–178, https://doi.org/10.1016/0169-8095(93)90002-6,
1993.
Stewart, R. E., Isaac, G. A., and Shaw, R. W.: Canadian Atlantic Storms
Program: The meteorological field project, B. Am.
Meteorol. Soc., 68, 338–345,
https://doi.org/10.1175/1520-0477(1987)068<0338:casptm>2.0.co;2,
1987.
Stewart, R. E., Bachand, D., Dunkley, R., Giles, A., Lawson, B., Legal, L.,
Miller, S., Murphy, B., Parker, M., Paruk, B., and Yau, M.: Winter storms
over Canada, Atmos.-Ocean, 33, 223–247,
https://doi.org/10.1080/07055900.1995.9649533, 1995a.
Stewart, R. E., Yui, D. T., Chung, K. K., Hudak, D. R.,
Lozowski, E. P., Oleskiw, M., Sheppard, B. E., and Szeto, K. K.: Weather
conditions associated with the passage of precipitation type transition
regions over Eastern Newfoundland, Atmos.-Ocean, 33, 25–53, 1995b.
Stewart, R. E., Szeto, K. K., Bonsal, B. R., Hanesiak, J. M., Kochtubajda, B., Li, Y., Thériault, J. M., DeBeer, C. M., Tam, B. Y., Li, Z., Liu, Z., Bruneau, J. A., Duplessis, P., Marinier, S., and Matte, D.: Summary and synthesis of Changing Cold Regions Network (CCRN) research in the interior of western Canada – Part 1: Projected climate and meteorology, Hydrol. Earth Syst. Sci., 23, 3437–3455, https://doi.org/10.5194/hess-23-3437-2019, 2019.
Stuart, R. and Isaac, G.: Freezing precipitation in Canada,
Atmos.-Ocean, 37, 87–102, https://doi.org/10.1080/07055900.1999.9649622, 1999.
Takeuchi, Y., Kodama, Y., and Ishikawa, N.: The thermal effect of melting
snow/ice surface on lower atmospheric temperature, Arct. Antarct.
Alp. Res., 34, 20–25, https://doi.org/10.2307/1552504, 2002.
U.S. Army Corps of Engineers: Snow hydrology: Summary report of the snow
investigations, North Pacific Division, Portland, Ore, 437 pp., 1956.
Vincent, L. A., Zhang, X., Brown, R. D., Feng, Y., Mekis, E., Milewska, E.
J., Wan, H., and Wang, X. L.: Observed trends in Canada's climate and
influence of low-frequency variability modes, J. Climate, 28,
4545–4560, https://doi.org/10.1175/jcli-d-14-00697.1, 2015.
Vincent, L. A., Zhang, X., Mekis, E., Wan, H., and Bush, E. J.: Changes in
Canada's climate: Trends in indices based on daily temperature and
precipitation data, Atmos.-Ocean, 56, 332–349,
https://doi.org/10.1080/07055900.2018.1514579, 2018.
Wang, X. L.: Climatology and trends in some adverse and fair weather
conditions in Canada, 1953–2004, J. Geophys. Res., 111, D09105,
https://doi.org/10.1029/2005JD006155, 2006.
Wasserstein, R. L., Schirm, A. L., and Lazar, N. A.: Moving to a world beyond
“p < 0.05”, Am. Stat., 73, 1–19, 2019.
Wexler, R., Reed, R. J., and Honig, J.: Atmospheric cooling by melting snow,
B. Am. Meteorol. Soc., 35, 48–51,
https://doi.org/10.1175/1520-0477-35.2.48, 1954.
WMO (World Meteorological Organization): International Cloud Atlas Manual on the
Observation of Clouds and Other Meteors, (WMO-No. 407), available at:
https://cloudatlas.wmo.int/home.html (last access: 1 April 2020), 2017.
Yang, D., Goodison, B. E., Metcalfe, J. R., Golubev, V. S., Elomaa, E.,
Gunther, T., Bates, R., Pangburn, T., Hanson, C., Emerson, D., Copaciu, V.,
and Milkovic, J.: Accuracy of Tretyakov precipitation gauge: Result of WMO
intercomparison, Hydrol. Process., 9, 877–895,
https://doi.org/10.1002/hyp.3360090805, 1995.
Yang, D., Goodison, B. E., Metcalfe, J. R., Golubev, V. S., Bates, R.,
Pangburn, T., and Hanson, C. L.: Accuracy of NWS 8” standard nonrecording
precipitation gauge: Results and application of WMO Intercomparison, J.
Atmos. Ocean. Tech., 15, 54–68,
https://doi.org/10.1175/1520-0426(1998)015<0054:AONSNP>2.0.CO;2, 1998.
Zhang, X., Vincent, L. A.,
Hogg, W., and Niitsoo, A.: Temperature and precipitation trends in Canada
during the 20th century, Atmos.-Ocean, 38, 395–429,
https://doi.org/10.1080/07055900.2000.9649654, 2000.
Zhang, X., Brown, R., Vincent, L., Skinner, W., Feng, Y., and Mekis, É.: Canadian climate trends, 1950–2007, Canadian biodiversity: Ecosystem status and trends 2010, (Technical Thematic Report No. 5), Canadian Councils of Resource Ministers, Ottawa, Ontario, iv +21 pp., available at: http://www.biodivcanada.ca/default.asp?lang=En&n=137E1147-0 (last access: 2 April 2020), 2011.
Short summary
This article provides a Canada-wide analysis of near-0°C temperature conditions (±2°C) using hourly surface temperature and precipitation type observations from 92 locations for the 1981–2011 period. Higher annual occurrences were found in Atlantic Canada, although high values also occur in other regions. Trends of most indicators show little or no change despite a systematic warming over Canada. A higher than expected tendency for near-0°C conditions was also found at some stations.
This article provides a Canada-wide analysis of near-0°C temperature conditions (±2°C) using...
