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  • 1
    Publication Date: 2023-10-24
    Description: Trends in flood magnitudes vary across the conterminous USA (CONUS). There have been attempts to identify what controls these regionally varying trends, but these attempts were limited to certain—for example, climatic—variables or to smaller regions, using different methods and datasets each time. Here we attribute the trends in annual maximum streamflow for 4,390 gauging stations across the CONUS in the period 1960–2010, while using a novel combination of methods and an unprecedented variety of potential controlling variables to allow large‐scale comparisons and minimize biases. Using process‐based flood classification and complex networks, we find 10 distinct clusters of catchments with similar flood behavior. We compile a set of 31 hydro‐climatological and land use variables as predictors for 10 separate Random Forest models, allowing us to find the main controls the flood magnitude trends for each cluster. By using Accumulated Local Effect plots, we can understand how these controls influence the trends in the flood magnitude. We show that hydro‐climatologic changes and land use are of similar importance for flood magnitude trends across the CONUS. Static land use variables are more important than their trends, suggesting that land use is able to attenuate (forested areas) or amplify (urbanized areas) the effects of climatic changes on flood magnitudes. For some variables, we find opposing effects in different regions, showing that flood trend controls are highly dependent on regional characteristics and that our novel approach is necessary to attribute flood magnitude trends reliably at the continental scale while maintaining sensitivity to regional controls.
    Description: Key Points: A wide variety of controls are necessary to explain flood magnitude trends across the United States between 1960 and 2010. Climatic changes and land cover conditions are of similar importance for flood magnitude trends at the regional scale. Controls on flood trends can have highly nonlinear effects and can have opposing effects in different hydro‐climatological subregions.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: USACE Water Institute
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: https://nwis.waterdata.usgs.gov/usa/nwis/peak
    Description: https://water.usgs.gov/GIS/metadata/usgswrd/XML/streamgagebasins.xml
    Description: https://psl.noaa.gov/
    Description: https://www.sciencebase.gov/catalog/item/59692a64e4b0d1f9f05fbd39
    Keywords: ddc:551.48 ; annual maximum flood ; magnitude trends ; drivers ; Random Forest ; clustering ; climate change
    Language: English
    Type: doc-type:article
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  • 2
    Publication Date: 2021-07-04
    Description: Since 2002, there has been a clear increase in Indian summer monsoon rainfall (ISMR). We demonstrate that this increase is associated with a change in the dynamics of the Intertropical Convergence Zone (ITCZ). Using a recently released reanalysis product from 1980–2016, we show that the ITCZ has strengthened and propagated northward since 2002. Analysis of the total energy budget reveals an increase in energy divergence and atmospheric diabatic heating, which is consistent with the changes in the ITCZ. Although global aerosol optical depth shows a significant positive trend during 1980–2016, it has declined over many parts of India since 2002. We put forward the hypothesis that this is the driver of the changing characteristics of the ITCZ. Our results suggest that changes in the dynamics of the ITCZ, together with changes in the energy/moisture budget, are responsible for the strengthening of ISMR since 2002, consistent with the emergence of a greenhouse gas‐induced signal.
    Description: Plain Language Summary: Indian summer monsoon rainfall (ISMR) is a major component of the Asian summer monsoon, providing 80% of the total annual rainfall in India. Even a small deviation of ISMR from normal has a significant effect on the Indian economy. Thus, understanding the dynamics of ISMR is of critical importance. During the latter part of the 20th century, ISMR experienced a significant reduction in its magnitude, with multiple hypotheses proposed to explain this weakening. However, we show that since 2002, there has been a clear increase in the magnitude of ISMR. We propose that this increase in magnitude is associated with the strengthening and northward propagation of the Intertropical Convergence Zone (ITCZ). Further analysis reveals that aerosol optical depth has decreased over many parts of India since 2002. Therefore, we hypothesize that the reduced aerosol emissions have played a significant role in the revival of ISMR since that time.
    Description: Key Points: The dynamics of the Intertropical Convergence Zone has a significant role in changing the characteristics of the Indian monsoon rainfall. Since 2002, the ITCZ has strengthened and propagated northward, thereby increasing the magnitude of the Indian monsoon rainfall. The reduced aerosol emissions is the main driver of the changing characteristics of ITCZ, which caused the revival of monsoon rainfall.
    Description: Fulbright‐Kalam climate fellowship
    Description: Natural Environment Research Council (NERC) http://dx.doi.org/10.13039/501100000270
    Keywords: 551.6 ; Indian subcontinent ; Monsoon rainfall ; drying
    Type: article
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  • 3
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2015]. This is the author's version of the work. It is posted here by permission of National Academy of Sciences for personal use, not for redistribution. The definitive version was published in Proceedings of the National Academy of Sciences of the United States of America 112 (2015): 4576–4581, doi: 10.1073/pnas.1422270112.
    Description: Assessing temporal variability in extreme rainfall events prior to the historical era is complicated by the sparsity of long-term ‘direct’ storm proxies. Here we present a 2200-yr-long, accurate and precisely dated record of cave flooding events from the northwest Australian tropics that we interpret, based on an integrated analysis of meteorological data and sediment layers within stalagmites, as representing a proxy for extreme rainfall events derived primarily from tropical cyclones (TCs) and secondarily from the regional summer monsoon. This time series reveals substantial multi-centennial variability in extreme rainfall, with elevated occurrence rates characterizing the twentieth century, the period 850-1450 CE, and 50-400 CE; reduced activity marks 1450-1650 CE and 500-850 CE. These trends are similar to reconstructed numbers of TCs in the North Atlantic and Caribbean basins, and form temporal and spatial patterns best explained by secular changes in the dominant mode of the El Niño-Southern Oscillation (ENSO), the primary driver of modern TC variability. We thus attribute long-term shifts in cyclogenesis in both the central Australian and North Atlantic sectors over the past two millennia to entrenched El Niño or La Niña states of the tropical Pacific. The influence of ENSO on monsoon precipitation in this region of northwest Australia is muted, but ENSO-driven changes to the monsoon may have complemented changes to TC activity.
    Description: Funding was provided by the Paleo Perspectives on Climate Change (P2C2) program of the United States National Science Foundation (NSF) through grant AGS-1103413, a seed grant from the Center for Global and Regional Environmental Research, and Cornell College (all to R.D.), the Kimberley Foundation Australia (to K-H.W.), and Penzance and John P. Chase Memorial Endowed Funds at WHOI (to C.U.).
    Description: 2015-09-30
    Keywords: Speleothem ; Tropical cyclone ; Monsoon ; El Niño/Southern Oscillation ; Australia
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 4
    Publication Date: 2022-05-25
    Description: © The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 6 (2016): 34485, doi:10.1038/srep34485.
    Description: The seasonal north-south migration of the intertropical convergence zone (ITCZ) defines the tropical rain belt (TRB), a region of enormous terrestrial and marine biodiversity and home to 40% of people on Earth. The TRB is dynamic and has been shown to shift south as a coherent system during periods of Northern Hemisphere cooling. However, recent studies of Indo-Pacific hydroclimate suggest that during the Little Ice Age (LIA; AD 1400–1850), the TRB in this region contracted rather than being displaced uniformly southward. This behaviour is not well understood, particularly during climatic fluctuations less pronounced than those of the LIA, the largest centennial-scale cool period of the last millennium. Here we show that the Indo-Pacific TRB expanded and contracted numerous times over multi-decadal to centennial scales during the last 3,000 yr. By integrating precisely-dated stalagmite records of tropical hydroclimate from southern China with a newly enhanced stalagmite time series from northern Australia, our study reveals a previously unidentified coherence between the austral and boreal summer monsoon. State-of-the-art climate model simulations of the last millennium suggest these are linked to changes in the structure of the regional manifestation of the atmosphere’s meridional circulation.
    Description: Funded by grants from the US National Science Foundation (NSF) Paleo Perspectives on Climate Change (P2C2) program (AGS-1103413), the Center for Global and Regional Environmental Research, and Cornell College (to R.F.D.); and the NSF P2C2 program (AGS-1203704 and AGS-1602455) and the Penzance and John P. Chase Memorial Endowed Funds at WHOI (to C.C.U.).
    Repository Name: Woods Hole Open Access Server
    Type: Article
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