Relevant bibliographies by topics / Droughts

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Droughts'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 July 2025

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Journal articles on the topic "Droughts"

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Tan, Xuwei, Qian Zhao, Yanlan Liu, and Xueru Zhang. "DroughtSet: Understanding Drought Through Spatial-Temporal Learning." Proceedings of the AAAI Conference on Artificial Intelligence 39, no. 27 (2025): 28440–48. https://doi.org/10.1609/aaai.v39i27.35066.

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Drought is one of the most destructive and expensive natural disasters, severely impacting natural resources and risks by depleting water resources and diminishing agricultural yields. Under climate change, accurately predicting drought is critical for mitigating drought-induced risks. However, the intricate interplay among the physical and biological drivers that regulate droughts limits the predictability and understanding of drought, particularly at a subseasonal to seasonal (S2S) time scale. While deep learning has demonstrated the potential to address climate forecasting challenges, its a
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Jedd, Theresa, Deborah Bathke, Duane Gill, et al. "Tracking Drought Perspectives: A Rural Case Study of Transformations Following an Invisible Hazard." Weather, Climate, and Society 10, no. 4 (2018): 653–72. http://dx.doi.org/10.1175/wcas-d-17-0067.1.

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Abstract Rural towns are especially susceptible to the effects of drought because their economies are dependent on natural resources. However, they are also resilient in many ways to natural hazards because they are rich in civic engagement and social capital. Because of the diverse nature of drought’s impacts, understanding its complex dynamics and its effects requires a multidisciplinary approach. To study these dynamics, this research combines appreciative inquiry, the Community Capitals Framework, and a range of climatological monitoring data to assess the 2012–14 Great Plains drought’s ef
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Teweldebirhan Tsige, Dawit, Venkatesh Uddameri, Farhang Forghanparast, Elma Annette Hernandez, and Stephen Ekwaro-Osire. "Comparison of Meteorological- and Agriculture-Related Drought Indicators across Ethiopia." Water 11, no. 11 (2019): 2218. http://dx.doi.org/10.3390/w11112218.

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Meteorological drought indicators are commonly used for agricultural drought contingency planning in Ethiopia. Agricultural droughts arise due to soil moisture deficits. While these deficits may be caused by meteorological droughts, the timing and duration of agricultural droughts need not coincide with the onset of meteorological droughts due to soil moisture buffering. Similarly, agricultural droughts can persist, even after the cessation of meteorological droughts, due to delayed hydrologic processes. Understanding the relationship between meteorological and agricultural droughts is therefo
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Chartier-Rescan, Corentin, Raul R. Wood, and Manuela I. Brunner. "Snow drought propagation and its impacts on streamflow drought in the Alps." Environmental Research Letters 20, no. 5 (2025): 054032. https://doi.org/10.1088/1748-9326/adc824.

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Abstract Snow droughts, that is negative anomalies in annual snow storage, challenge water resources management in snow-rich catchments and their downstream regions because they can lead to succeeding streamflow droughts in the following melt season. Under continued global warming, snow droughts are expected to become more frequent and intense, which likely increases the occurrence of succeeding streamflow droughts. However, we still know little about the rate at which snow droughts propagate to subsequent streamflow droughts, the spatial patterns of these concurrent events, the influence of s
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Li, Zhuoyuan, Er Lu, Juqing Tu, and Dian Yuan. "Historical and Future Changes in Meteorological–Hydrological Compound Drought in China." Atmosphere 15, no. 12 (2024): 1459. https://doi.org/10.3390/atmos15121459.

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Drought is typically divided into meteorological, agricultural, hydrological, and socioeconomic categories. Generally, the transition from meteorological drought to other types of droughts is known as drought propagation. When drought propagation occurs, different types of droughts may still exist simultaneously or successively. In this study, compound droughts are divided into three categories: hydrological meteorological compound drought (HMD), meteorological hydrological compound drought (MHD), and simultaneous compound drought (SD). ERA5 and CMIP6 data are used for analysis under historica
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He, Yuanhuizi, Fang Chen, Huicong Jia, Lei Wang, and Valery G. Bondur. "Different Drought Legacies of Rain-Fed and Irrigated Croplands in a Typical Russian Agricultural Region." Remote Sensing 12, no. 11 (2020): 1700. http://dx.doi.org/10.3390/rs12111700.

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Droughts are one of the primary natural disasters that affect agricultural economies, as well as the fire hazards of territories. Monitoring and researching droughts is of great importance for agricultural disaster prevention and reduction. The research significance of investigating the hysteresis of agricultural to meteorological droughts is to provide an important reference for agricultural drought monitoring and early warnings. Remote sensing drought monitoring indices can be employed for rapid and accurate drought monitoring at regional scales. In this paper, the Moderate Resolution Imagin
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Lee, Sang-Min, Hi-Ryong Byun, and Hiroshi L. Tanaka. "Spatiotemporal Characteristics of Drought Occurrences over Japan." Journal of Applied Meteorology and Climatology 51, no. 6 (2012): 1087–98. http://dx.doi.org/10.1175/jamc-d-11-0157.1.

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AbstractThe drought climate of Japan from 1902 to 2009 was analyzed using an effective drought index (EDI). Drought regions were identified by hierarchical cluster analysis using drought characteristics (duration, severity, and onset and end dates) obtained from 50 observation stations. The results indicated that droughts could be divided into four groups (G1–G4) that reflected the local climate. The four groups were related to precipitation as follows. The summer rainy season affected groups G2–G4, in which droughts occurred mainly during spring and summer and were relieved before and after t
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Liu, Kuan, Buliao Guan, Jiaqi Zhai, et al. "Characteristics and Lag Time of Meteorological Drought Propagation to Hydrological Drought in the Haihe River Basin." Sustainability 17, no. 11 (2025): 5134. https://doi.org/10.3390/su17115134.

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Understanding the propagation dynamics from meteorological to hydrological droughts, particularly in regions heavily influenced by human activities, is essential for the effective monitoring and prevention of hydrological drought risks. This study focuses on the Haihe River Basin, investigating the evolution of meteorological and hydrological droughts using the Standardized Precipitation and Evapotranspiration Index and the Standardized Runoff Index, supplemented by run theory analysis. Using correlation analysis, we examine the propagation lag times between meteorological and hydrological dro
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Kim, Woon Mi, and Christoph C. Raible. "Dynamics of the Mediterranean droughts from 850 to 2099 CE in the Community Earth System Model." Climate of the Past 17, no. 2 (2021): 887–911. http://dx.doi.org/10.5194/cp-17-887-2021.

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Abstract. In this study, we analyze the dynamics of multi-year droughts over the western and central Mediterranean for the period of 850–2099 CE using the Community Earth System Model version 1.0.1. Overall, the model is able to realistically represent droughts over this region, although it shows some biases in representing El Niño–Southern Oscillation (ENSO) variability and mesoscale phenomena that are relevant in the context of droughts over the region. The analysis of the simulations shows that there is a discrepancy among diverse drought metrics in representing duration and frequencies of
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Bae, Hyedeuk, Heesook Ji, Yoon-Jin Lim, Young Ryu, Moon-Hyun Kim, and Baek-Jo Kim. "Characteristics of drought propagation in South Korea: relationship between meteorological, agricultural, and hydrological droughts." Natural Hazards 99, no. 1 (2019): 1–16. http://dx.doi.org/10.1007/s11069-019-03676-3.

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Abstract To investigate the propagation of meteorological droughts to agricultural and hydrological droughts, the relationship between droughts was analyzed using observed precipitation and agricultural reservoir and dam storage levels with SPI from 1998 to 2015 in South Korea. For the relationship between different types of droughts, we find that the occurrence of meteorological droughts after concentrated precipitation in the wet season (from June to September) tends not to lead to agricultural or hydrological droughts. A lack of precipitation from April to September, when large volumes of i
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Dissertations / Theses on the topic "Droughts"

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Quiring, Steven M. "Developing a real-time agricultural drought monitoring system for Delaware." Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file 2.86 Mb , 207 p, 2005. http://wwwlib.umi.com/dissertations/fullcit/3181867.

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Guinan, Patrick E. "Seasonally adjusted index for projecting agricultural drought /." free to MU campus, to others for purchase, 2004. http://wwwlib.umi.com/cr/mo/fullcit?p3164510.

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Bellamy, John Thomas. "Drought frequency and risk analysis in the Upper Green River Basin, Wyoming." Laramie, Wyo. : University of Wyoming, 2008. http://proquest.umi.com/pqdweb?did=1798480881&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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Dube, Carolina. "The impact of Zimbabwe's drought policy on Sontala rural community in Matabeleland South Province /." Link to the online version, 2008. http://hdl.handle.net/10019/1768.

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Chbouki, Nabil. "Spatio-temporal characteristics of drought as inferred from tree-ring data in Morocco." Diss., The University of Arizona, 1992. http://hdl.handle.net/10150/185851.

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Long-term tree-ring series of Cedrus atlantica have been utilized to reconstruct and characterize past drought occurrences in Morocco. Based on the close relationship between tree growth and rainfall variations, the best tree-ring indicator of drought has been found to be, x₀ = μ -.75σ, with μ and σ the mean and standard deviation of the tree-ring series. In Morocco, drought is a short event lasting 1.7 years on average with 84% of the events lasting less than 2 years. The average maximum duration exceeds 4 years. It is associated with a 40% deficit about normal moisture availability which can
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Kebede, Yohannes. "Economic evaluation of post-drought recovery agricultural project : the case of Tegulet and Bulga District, Shoa Province, Ethiopia." Thesis, McGill University, 1988. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63894.

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Singh, Kamal. "Drought, relief and rural communities : special report no. 9." Association for Rural Advancement (AFRA), 1993. http://hdl.handle.net/10962/68651.

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The Association for Rural Advancement (AFRA) has run a Drought Project since October 1992. The project's primary focus was to monitor drought conditions in the AFRA's operational area and to assist communities to access relief through providing them with relevant information and helping them to submit proposals to relief agencies. In attempting to do this, it became clear that the effects of drought on rural black communities was not a well understood phenomenon. We also found that relief strategies were informed more by economic, agricultural and meteorological criteria than social ones. This
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Rudebeck, Hugo. "HYDROLOGICAL DROUGHTS IN SWEDEN: Mapping of historical droughts and identificationof primary driving climate variables andcatchment properties." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-350520.

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This study investigated the relationship between hydrological, and to some extent, meteorological droughts, and meteorological variables and catchment characteristics in 235 Swedish catchments between 1983 and 2013. This was done in order to investigate what factors affect the drought sensitivity in Swedish catchments and to map the occurrence of droughts in Sweden between 1983 and 2013. There have been studies about which meteorological phenomena and catchment characteristics that promote hydrological droughts, but for Sweden this is relatively unexplored. To investigate droughts during the s
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Ren, Xiaomeng, and University of Lethbridge Faculty of Arts and Science. "Agricultural vulnerability to drought in southern Alberta : a quantitative assessment." Thesis, Lethbridge, Alta. : University of Lethbridge, Faculty of Arts and Science, 2007, 2007. http://hdl.handle.net/10133/398.

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Agricultural vulnerability is generally referred to as the degree to which agricultural systems are likely to experience harm due to a stress. In this study, an existing analytical method to quantify vulnerability was adopted to assess the magnitude as well as the spatial pattern of agricultural vulnerability to varying drought conditions in Southern Alberta. Based on the farm reported data and remote sensing imagery, two empirical approaches were developed to implement vulnerability assessment in Southern Alberta at the quarter-section and 30 meter by 30 meter pixel levels. Cereal crop yield
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Stockton, Charles W., David M. Meko, and William R. Boggess. "Drought History and Reconstructions from Tree Rings." Laboratory of Tree-Ring Research, University of Arizona (Tucson, AZ), 1989. http://hdl.handle.net/10150/302684.

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Books on the topic "Droughts"

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Karanth, G. K. Surviving droughts. Himalaya Pub. House, 1995.

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Franchino, Vicky. Droughts. Cherry Lake Pub., 2012.

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Scheff, Duncan. Droughts. Raintree, 2003.

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Inc, World Book, ed. Droughts. 2nd ed. World Book, 2009.

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B, Fradin Dennis, ed. Droughts. National Geographic, 2008.

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ill, Ceolin Andre, ed. Droughts. HarperCollins Publishers, 2017.

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Park, Louise. Droughts. Smart Apple Media, 2007.

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Allaby, Michael. Droughts. Facts On File, 1998.

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Fradin, Judith Bloom. Droughts. National Geographic, 2008.

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Wendorff, Anne. Droughts. Bellwether, 2008.

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Book chapters on the topic "Droughts"

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Tian, Guoliang, and Vijendra K. Boken. "Monitoring Agricultural Drought in China." In Monitoring and Predicting Agricultural Drought. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780195162349.003.0039.

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Droughts account for more than half of the total number of natural disasters faced by China. Serious droughts impact industrial production, water supply, people’s lives, and the ecological environment, which causes significant losses to the national economy. Because of increasing water shortages, drought has become one of the most important factors that limits agricultural production, especially in the north where droughts occur frequently. According to the Chinese terminology, if reduction in crop yields in an area is more than three-tenths of the average, the area is called a “damaged area,”
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"PROSPECTS FOR THE PREDICTION OF METEOROLOGICAL DROUGHT." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-36.

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"that c p ef ofsotr -t dsisoausltderbeemeu rg se e d to minimi and optimise n cy th ree li uesfe an o d se frreeh devas caebnitl it taatt te iionng nological advancements in climate-based tech­ nologies for drought monitoring, diagnosis, and p in rveeds ic tm tio en n t . s H in o w se ecv to erra , l K pr eendyias as h te arspm la andne in gmaanndy m me anntasg em th eanttahcatv iv e itie bse . enT he m se adien clu at det the invest­ he Kenya M Me otneiotroorlionggicC al e D nt e re paarn tm deinntaagnrdicRue lt guiroanlaalnDdrowuagth er t resources activities, among many other sectors. aSvuocihdesfe fo ct r o ts r al m ust, however, be integrated to drought prepared cnoens fl sic ‘ tsshoacnkda bs p o ro rb v e id rs e ’ . effective ----- i -." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-66.

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"AN ASSESSMENT OF THE DROUGHT HAZARD IN MOROCCO." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-86.

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"icnodm ic persehceannsb iv e e fo ruen vi dew in aof te cdhrnoiucg al htnod te efp in uib ti l o is nhsedanbdytuhsiusaltliyme ta kpee ri tohd re ceanorvam ry orceonm si odn er tahbs ly t , o develop, but t ( h1e9 75 W ). o O rld th er Mseotuerocreosl , osguicchalasSOurbgraanhim za atn io ynam ( ( W 19 M 67 O ) ) , d th e e fi ci teinmciyn . gFoorfextahmep le in , i a ti a si t g io n n if ic o an f the de p p re ecnidpiin ta gtioonndGl. l an (1 tz 98a0n ) d , K an at dzW (1 i 9 lh 7i7 te ), aSnadndG fo lradnt ( z19 ( 7199 ) 8 , 5 D ), raccaunpbeetm th aenywilnotcearlesse . as Hoonwm ev aeyr have few, itfdarnyyp , eriod during consulted for a thorough discussion of the difficulties into the growing seaso , n , ifth th eisim de pfaicctisenm cy im cpoancttisnufeosr in dDer fi onu in gghtdrhoausghbte . en grouped by type as follows: w qu iinctkelrysseianscoenlroew su l p ts r ec in ip itation during th ay magnify meteorological, hydrological, agricultural, and socio­ rates, leading to deficien lo twsosiol il mmoo is itsutruereerfeac ll haarngdeeex co pl nao in msic th e ( W re illahtiitoensahnidpbGeltawnetezn1 th 9e8s5e ) . vaF ri ioguusret yp 1 e .4 s pla M nti entg. at spring of drought and the duration of the event. Droughts express eeodro so lo le gliycaolnt ( hoer ba csliismo at fotlhoegidceagl) r ee droofudgrh yn t es iss." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-28.

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"tboeo tw leoenngtfhorresah ll olddateevs en otfs th a e re s e to e o ve nsthsorttoabnedeoqtuhaelr ly s c (N on ota in hueefd fe c th t) r o (F uigghuo re ut2 . t2h , e to r p em ). Precipita likely. This indicates a tendenc ainder of titohned1 ef 9i7 ci 0tssf0e . r3e7nt ( 5clp im er atcee ’ n . Atcvoanlfuiedeonfc ( eDv si a g lu nyeifitcoanp tl eyrisom ds a l of ‘dif­ and 1980s and well into the 1990s (Joseph effect), implies tha for n = 40 ilser0t . h3a0n ) p (F ro ig v u id re in g 2 .2 a , ‘n beow tt om cli ) m . a F te u ’ rt fhoerrtdhies cu wse si s o te nrnofSathheelu sp su ac al eldyfro ef rlteac ll the tdsa te dat hor s t -t eosboefe th qu e events are too regularly Sherman statistic is given in Folland and." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-38.

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"eppeirsocdeenst . oTfhtehequm as oir -e glm ob aarlkesd ca lEeN se SaO warm ture (SST) patterns associated wistuhr fa E ce Ntaenmdpceorlad ­ R bution of rainfall as a functio SO that sta ogpees le w of skEiNaSnOdcHaanlpoefr te tn1b9e9no5i ) d . efBEeNcS au Ose st tah te e ( eea .g., influence these rainfall patterns appear consistently in more before typical ENSO-ntified a season r o ly rfmoarnryecreencten de tcsa tu d d es ie , s P -ar kee .g r ., anHdsF iu o n ll ganadnd19N9e1wseilnlc1e9t8h3ereepc is oogdneith io ansiomfp th oer ta e n ar tlyprsetdarg el easteodfdarodu ev gehltospcionmgm EN en ScOe, late Idne in nt eitfe ic eanttihonc entury. However, one of th ic e t ive m value. precipitation relatio onfs hip tshepsreo vid ceo ain limitations sntsh is etecnlte are E st NiSnO di -­ E ac NcS or O d -in b g as teod th s e ea h so is ntaolr ic parlerdeicco ti rodn , EsN ch SeOmeissaicst iv tehaot, fce ation that seasonal meteorological drought in quite its warm or cold phases only about half the tim ienux se te fnuslisvkei ll a r ( e i. aes , ionftthheehg is lo to bre ic m al aryecboerdp , reEdN ic S ta O b -l reelw at i e th d S co in ld ce 1e9p0 is 0 o , dteh er yeeahrasv , e b ac eceonrtdhiinrg ty w to a rm th aendSnoiunteh te e e rn n . idtnryth con he aepspedroa it prie on r a ia s s ). occu te Fsiegaursroeat2 leas ns, .3 whsth7o5wsp ere p e th rocse recip entre of the time Osc itatio gi nondse , fiacn it dsJSoonue il s l at ( i1o9n87 In ) dex-based criterion of Ropelewski and are strongly associated with the warm or cold phase equa th to errinalPOas . c The cif il ilca tio clos se n a su Iendreex la tio (S n O sh I i ) pbaentdw ee cne nt trhaelo tu freEsNiSnOth -e i t . reo ., piw ca alrm ea sotrPcaoclid fi c s . eaAlstuhro face tempera­ d rface temperature anomaly may not occur consistently with every wuagrhmdorroucgoh ld tFu ig r u in durin re ggm2.4o all . s t su Ioffptr he twentieth century is illustrated in ENSO episode as appropriate, these regions do have a dr ch E ec N ip SiO ta ti eopn is owdeerse , sbku il tfun ll oytportehdeircw ta ibslee , tch le aanr -l n y or i m de anltsie fi aesdo na ilncco re nadsie ti d o ns p . r T ob haebliiln it k y wi o th fEdN ri SeOr-r th es eouotuigrm ht p ce e s . H re odw ic etv io enw managed r, ecvroouplsdm on ulsytbbeeppolsasnitbeldeaabnoduwtahtaelrfcba il n it ybedifso tr rim bu al tiisoend by ca ery year. s condi ltciuolnaatl in ognptrheecisptiattaet io onfEpN ro SbOa . ­ m ho awneyvedrr , ouEgNhSt-Op ro is nenortegtihoensonAlsy is disc . The farce to la r u ssed tiv in el f y lu ebnec lo in w g , T hi h st uosripcrae ll c y ip o it bas ti eornvepdr edic recent shif ttison in sctahnebperobb as aebd il iptuyredliysto ri n ­ g at a m in ossipnhu er nedesryssttaenmditnhg ro oufgch li m EN ate S O as satucdoiueps le h d as olceedan to -." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-40.

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"tcoourpulnedexopceenasn iv -a etm en ossepmhbelrees . mIofdseol , s w to ecpo re u d ld ic tuslea rg th e e -l doiscst . i on Tsh , ebasskeid ll in seasonal rainfall and f scale indices such as the SOI, then use statistical generated the v o al nuethferoEmlN us iinnog -S ta ocu ti tchaelrnmaOnsrcoisltl at p io rne , ­ v re alra ia ti bolne ships between these forec agement. fic locat siowne . nAele te drn to at p iv reeldyi , ctw , esuccohuaasstraii ndices and the This study demonstrated that the skill obtainable in models to ld us nefatlhleatcaosuppelceid ­ A gr uosu tr nad li s a , th weaisrussueffiinc ie c n ro tptmo an ju asg ti efmy, enot. n Pr eecsounmoam bl iycp en re s d em ic b te lderpurnesdiocftasneaas tm ur o fa scpehetreimc peratures, then use these forecasts could also be useful in drought-dicti sea surface temperature msotdoelpfro ep rc aerdew pr it e h ­ mmiannaatg io enmeonftadpep ci rsoiporniam te aksitnogc , kifnogrirnas te ta sncoen in padse to te ra r l ­ tChoenbsoi ns edse of trsatbrlera ate tihno fa gy ulglhatnadndotthee st rinvga riables of interest. properties (McKeon et al. 1990). prediction. for using models iisnnseeead so endaltoc li s m el aetcet." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-55.

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"JDaenvee ir loop ( mBe ra nzt (UNCED), which was held in Rio de and 4.2d). Such complex spatial rain into the twe il n ) ty in -f iJrusntec1 en 99 tu 5 r . yUaN re CEsD um a m ct a io ri n se pdl an in s a se ls cot io cnomhm ig ohn li gdhu ts r in th g e an so ocm io a e lo cuosnorm ain ffaa ll llpyaeta te rs r . nsTahriestUoNaCsE ‘ D A ’ gsepnudba lic 2a1t \ io n T , h w re hei ch coinsvceonm tio mnosnlryel referred are often associat ic disasters that environmental degradation that were negotia at teeddb to y climatology of the eddrow ug it hhtsd is ropurg es hetns te idnfK irs etn . ya. The U Co NnCvE en D ti on in colnudCel im th a e te UCn ha it negdeN (U a N tio FnCsC Framework N (U a N tio CnCsD) C." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-61.

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"Oscillation) in the early." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-51.

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Conference papers on the topic "Droughts"

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Dimitrov, Yordan. "HYDROLOGICAL DROUGHT FREQUENCY ANALYSIS IN THE YANTRA RIVER DOWNSTREAM." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/3.1/s12.14.

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Hydrological droughts are formed by different processes, but how strong and heterogeneous they are, leading to different manifestation and characteristics of the droughts. Droughts have no distinct starting date, but different methods gives a course of action that may help to identify dry signals and possible drought conditions for early warning. We choose hydrological drought indices that are applicable for Bulgarian conditions. Using statistical methods, minimum flow, deficits and spatial characteristics can be evaluate, as well as identifying vulnerable river catchments and regions or affec
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Nikolova, Nina, Simeon Matev, Neli Hristova, and Kalina Radeva. "HYDROMETEOROLOGICAL DROUGHT IMPACT ON CEREAL PRODUCTION IN NORTHERN BULGARIA." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/3.1/s12.15.

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On the background of regional climate changes, an increase in the frequency and intensity of extreme droughts has been observed in many regions of Europe in recent years, and this trend is expected to continue in the future. While common in southern Europe, including Bulgaria, drought can adversely affect human life and economic activities. Extreme droughts lead to water scarcity, restricting the availability of irrigation water for agricultural purposes. In the regions where irrigation is vital for sustaining crop production, diminished water availability can result in crop failures and econo
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Safdarian, Farnaz, Jessica L. Wert, Dalton Cyr, and Thomas J. Overbye. "Power System Resiliency and Reliability Issues from Renewable Resource Droughts." In 2024 IEEE Kansas Power and Energy Conference (KPEC). IEEE, 2024. http://dx.doi.org/10.1109/kpec61529.2024.10676081.

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Dobiasova, Ivana, Martin Minarik, and Jan Jan. "CHANGE OF THE GROWING SEASON IN THE CONTEXT OF CLIMATE CHANGE IN SLOVAKIA." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024v/4.2/s18.26.

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Climate change significantly affects agriculture in Slovakia by altering precipitation patterns, temperatures, and the length of the growing season. Common effects include drought, more intense rainfall, higher summer temperatures, and increased pest populations, all of which influence crop production and livestock breeding. Human activities have already impacted atmospheric properties such as temperature, precipitation, CO2 levels, and ground-level ozone, and this trend is expected to continue. While warmer climates may benefit some crops, the increased frequency of droughts, floods, and heat
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Zhgun, Kseniia, Farnaz Safdarian, and Thomas J. Overbye. "Classification and Identification of Renewable Energy Droughts in the United States." In 2025 IEEE Texas Power and Energy Conference (TPEC). IEEE, 2025. https://doi.org/10.1109/tpec63981.2025.10907126.

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Aher, Anagha, Sonal Sonarghare, Janhavi Kasar, Aman Dhumal, Vedant Mayekar, and Aavani Nair. "Risk Assessment and Prediction of Floods and Droughts using Attention-LSTM." In 2025 3rd International Conference on Communication, Security, and Artificial Intelligence (ICCSAI). IEEE, 2025. https://doi.org/10.1109/iccsai64074.2025.11063911.

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Tsitsagi, Mariam, Ana Palavandishvili, and Zaza Gulashvili. "DROUGHT INDICES AND VIS-BASED CANOPY STATUS OF VINEYARDS." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/3.1/s12.11.

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The study aims to evaluate how droughts impact irrigated and non-irrigated vineyards by analysing the relationship between short-term drought and vegetation indices to identify areas irrigated from unofficial sources. The re-search area includes vineyards in Telavi municipality (eastern Georgia). RStudio was used to calculate SPI and SPEI (1- month and 3-month timescales) and EDI (daily) to measure the severity of the meteorological drought. The 27-year (1993�2020) data from a weather station in the study area included daily temperature and precipitation. Water stress in crops using Sentinel 2
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Kovacova, Viera. "COMPARISON OF TWO METHODS FOR ASSESSMENT OF PH-DEPENDING VALUES IN SURFACE WATER." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/3.1/s12.08.

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The recent advances in current status and major mechanisms of water quality worsening, assessment of evaluation criteria and the influencing factors were reviewed. The changes in the atmosphere, the periodicity of the occurrence of extreme hydrological situations has been increasing in recent years. In the natural conditions of Slovakia, periods without rain are lengthening and the incidence of precipitation of extreme intensity and abundance is increasing. Hydrological extremes are generally manifested in the form of floods and droughts. The increased incidence of drought is a new phenomenon.
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Pasquariello, Pamela, Guido Masiello, Carmine Serio, et al. "Water Deficit Indices to Monitor Forests' Response to Droughts and Heat Waves." In IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2024. http://dx.doi.org/10.1109/igarss53475.2024.10642580.

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Kang, Minsun, Seulchan Lee, and Minha Choi. "Role of Terrestrial Evapotranspiration on the Occurrence of Flash Droughts in Northeast Asia." In IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2024. http://dx.doi.org/10.1109/igarss53475.2024.10642479.

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Reports on the topic "Droughts"

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Ortiz, Raphaëlle, Anamaría Núñez, Corinne Cathala, Ana R. Rios, and Mauro Nalesso. Water in the Time of Drought II: Lessons from Droughts around the World. Edited by Raul Muñoz, Alfred Grunwaldt, and Claudia Calderón. Inter-American Development Bank, 2021. http://dx.doi.org/10.18235/0003425.

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This technical note is an update to the previous "Water in the Time of Drought: Lessons from Five Droughts Around the World", published in 2018. It explores drought situations and policies in Spain (including the Canary Islands), Chile, Mexico, the dry corridor between Honduras, Guatemala, and El Salvador, Brazil, and South Africa. Each of these countries has recently dealt with droughts and/or developed long-term solutions to manage them. HydroBID, a tool developed by the IDB, will be presented through relevant case studies. After defining drought experiences and institutional frameworks in e
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Cathala, Corinne, Anamaría Núñez, and Ana R. Rios. Water in the Time of Drought: Lessons from Five Droughts around the World. Inter-American Development Bank, 2018. http://dx.doi.org/10.18235/0001279.

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Núñez, Anamaría, Corinne Cathala, and Ana R. Rios. Water in the Time of Drought: Lessons from Five Droughts around the World. Inter-American Development Bank, 2018. http://dx.doi.org/10.18235/0008515.

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This policy brief examines these crises, explores successes and pitfalls in the response mechanisms, and extracts valuable lessons to assist decision makers in dealing with droughts, providing practical guidance in terms of urban planning and management. It will do so through a three-pronged approach: First, it describes the situation each utility and region faced while tackling the drought, as well as the measures they implemented to respond to that dire situation. Second, it will present some recommendations and lessons learned to build climate resilience in the future. Lastly, it will show
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Basani, Marcello, Raúl Muñoz Castillo, Giulia Carscasci, and Jihoon Lee. Piloting Drought Management Participatory Modeling-Based Approaches in Chile. Inter-American Development Bank, 2024. http://dx.doi.org/10.18235/0005500.

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Chile's unique geography and climatic zones, including the arid Atacama desert in the north and the cold, humid Patagonian zone in the south, represents a challenges for water resource management. Droughts, and particularly mega-droughts, have become more frequent and intense, affecting not only the north but also central regions like the Maipo basin basin, located in the Metropolitan Region. To address these issues, this project aims to develop a Drought Management Plan (DMP) for the Maipo basin, and to support analysis of drought conditions, including characterization of spatial coverage, in
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Costa, Flavia R. C., José Antonio Marengo, Ana Luisa M. Albernaz, et al. Policy Brief: Droughts in the Amazon. Sustainable Development Solutions Network (SDSN), 2024. http://dx.doi.org/10.55161/lvyb6857.

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Dorosh, Paul A., Jenny Smart, Bart Minten, and David Stifel. Droughts, cereal prices, and price stabilization options. International Food Policy Research Institute, 2020. http://dx.doi.org/10.2499/9780896296916_09.

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Ahmadi, Behzad. On the Drought Recovery and Resiliency: How Terrestrial and Riverine Ecosystems Recover from Agricultural and Hydrological Droughts. Portland State University Library, 2000. http://dx.doi.org/10.15760/etd.6710.

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Salimun, Ester. Southeast Asia braces for more droughts and haze. Edited by S. Vicknesan. Monash University, 2023. http://dx.doi.org/10.54377/28ac-037a.

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Landon-Lane, John, Hugh Rockoff, and Richard Steckel. Droughts, Floods and Financial Distress in the United States. National Bureau of Economic Research, 2009. http://dx.doi.org/10.3386/w15596.

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Sengupta, Sohini. How droughts can leave people with nowhere to go. Edited by Bharat Bhushan and Suzannah Lyons. Monash University, 2023. http://dx.doi.org/10.54377/375a-a279.

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