Special Issue "Hydroclimate in a Changing World: Recent Trends, Current Progress and Future Directions (2nd Edition)"

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Climatology".

Deadline for manuscript submissions: closed (30 November 2023) | Viewed by 695

Special Issue Editor

Lamont-Doherty Earth Observatory, Columbia University, New York, NY 10960, USA
Interests: climate variability and climate change; hydroclimate variability and change; droughts and floods; high-resolution numerical weather prediction
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Global warming is imposing tremendous challenges upon human lives and other lives on Earth, and people are working hard to find the causes and ways to adapt. We had a successful Special Issue on this topic last year, entitled “Hydroclimate in a Changing World: Recent Trends, Current Progress and Future Directions” (https://www.mdpi.com/journal/atmosphere/special_issues/hydroclimate_changing_world). However, more research results are waiting to be published, so we decided to run a second Special Issue on this topic. We sincerely welcome your contribution. A warmer atmosphere holds more moisture. The consensus is that the moisture transport via atmospheric circulation strengthens and makes already wet areas of moisture convergence wetter and already dry areas of moisture divergence drier. Therefore, the tropics and mid- to high latitudes will become wetter and the subtropics will become drier. Without any change in the interannual variability of the hydroclimate, the change in the mean hydroclimate would increase drought risk in some places and flood risk in other places. However, global warming will cause the interannual variability of the hydroclimate to intensify, which will induce more droughts and floods. Furthermore, the changing atmospheric circulation interaction with the land surface may cause the changing of storm tracks, and may play an important role in shaping moisture redistribution.

This Special Issue serves as a convenient platform for the community to document and discuss the hydroclimate response of global warming. Topics include, but are not limited to:

  • Diagnoses and forecasts of recent and future hydroclimatic extremes;
  • Hydroclimate dynamics;
  • Hydroclimate variability;
  • Food and water security under a changing climate;
  • Drought and flood under a changing climate.

Your participation is highly appreciated.

Dr. Haibo Liu
Guest Editor

Manuscript Submission Information

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Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Atmosphere is an international peer-reviewed open access monthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2400 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • forecast
  • climate variability
  • climate change
  • hydroclimate variability
  • droughts
  • floods
  • storms
  • storm track
  • precipitation
  • aridification

Published Papers (1 paper)

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Research

17 pages, 3364 KiB  
Article
Analysis of the Characteristics of Uneven Spatio-Temporal Distribution in Wujiang River Basin over the Last 60 Years
Atmosphere 2023, 14(9), 1356; https://doi.org/10.3390/atmos14091356 - 29 Aug 2023
Viewed by 444
Abstract
Exploring the characteristics of uneven temporal and spatial distribution of precipitation in mountain watersheds can provide a reference for regional agricultural development and resource utilization, and contribute to the protection of the ecological environment. Based on the daily precipitation observation data of 40 [...] Read more.
Exploring the characteristics of uneven temporal and spatial distribution of precipitation in mountain watersheds can provide a reference for regional agricultural development and resource utilization, and contribute to the protection of the ecological environment. Based on the daily precipitation observation data of 40 meteorological stations in the Wujiang River Basin from 1963 to 2021, the temporal- and spatial-variation characteristics of the precipitation concentration degree (PCD) and precipitation concentration period (PCP) were analyzed using the Randall S analysis method, Mann–Kendall test method, Pettitt method, wavelet analysis and empirical orthogonal function (EOF). The results showed that the fluctuation range of PCD in Wujiang River Basin from 1963 to 2021 was 0.34–0.59, with a multi-year average of 0.47, which was obviously higher than the national average level and is showing a trend of slowly increasing. The fluctuation range of PCP was between 17.1 and 21.5 days, with a multi-year average of 19.0. The annual precipitation was mostly concentrated around the middle of July and showed a slowly decreasing trend. The abrupt change in PCD and PCP occurred around 1983 and 2001, respectively. There is an obvious Hearst phenomenon in PCP. In the future, the trend of precipitation concentration in the middle period will remain in advance, and the degree of precipitation concentration will continue to increase. The maximum precipitation in the flood season will continue to be delayed. The spatial pattern of the first mode of PCD and PCP in the Wujiang River basin was consistent and showed an opposite pattern between the upper reaches and the middle-lower reaches of the basin, which reflects the influence of the topography of the basin on the spatial distribution of precipitation. The distribution of precipitation is affected by topography. The elevation change in the basin was complex, and the leeward slope varied a lot. Therefore, it has a significant impact on precipitation. Areas with less precipitation are at higher elevations and on mountain leeward slopes, with a lack of moist air flow. The area with more precipitation was the summer monsoon mountain windward slope, and the topography blocks the increase in precipitation. The elevation of the central region is relatively uniform and the terrain is flat. Therefore, the distribution of precipitation is more uniform. Full article
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