Assessing how accumulated precipitation and long dry sequences impact the soil water storage
ABSTRACT Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. The temporal and spatial variability of these variables, together with the evapotranspiration, is crucial in the east‐northeast of Argentina, where rain‐fed...
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description | ABSTRACT
Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. The temporal and spatial variability of these variables, together with the evapotranspiration, is crucial in the east‐northeast of Argentina, where rain‐fed agricultural production is carried out. In this work, the frequency of precipitation was studied from dry spells and complemented with an analysis of the accumulated precipitation and evapotranspiration. In particular, dry sequences longer than 15 days, return period and severity, were the focus of this study. Finally, the impact of the amount and frequency of precipitation on soil water storage was assessed through a decadal analysis. The region of study is characterized by northeast‐southwest gradient in accumulated precipitation and east–west gradient in winter long dry sequences. During summer, higher and more frequent precipitations (lower probability of long dry sequences and lower return period of 15 days and severity) were presented whereas the opposite was found in winter. However, the stations located to the west presented the highest probability of long dry sequences with higher severity and lower accumulated precipitation. This result highlights the vulnerability of the agriculture activity in the western stations. Regarding the impact of long dry sequences over soil water storage, the seasonality of evapotranspiration is also involved. The impact is stronger during austral summer because of higher values of evapotranspiration and it is lower during winter, in spite of the higher probability of long sequences. Decadal analysis suggested that soil water storage responds to precipitation amount or frequency depending on the magnitude of the anomalies. In this sense, the impact of precipitation over soil water storage depends on how it is distributed.
Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. In this research, long dry spells (longer than 15 days) and their impact on soil water storage were analysed in the eastern region of rain‐fed agriculture production of Argentina. The results highlight the vulnerability of the agriculture activity in the western stations and the role of evapotranspiration which enhances the effects of long dry spells in certain seasons. |
doi_str_mv | 10.1002/joc.5087 |
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Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. The temporal and spatial variability of these variables, together with the evapotranspiration, is crucial in the east‐northeast of Argentina, where rain‐fed agricultural production is carried out. In this work, the frequency of precipitation was studied from dry spells and complemented with an analysis of the accumulated precipitation and evapotranspiration. In particular, dry sequences longer than 15 days, return period and severity, were the focus of this study. Finally, the impact of the amount and frequency of precipitation on soil water storage was assessed through a decadal analysis. The region of study is characterized by northeast‐southwest gradient in accumulated precipitation and east–west gradient in winter long dry sequences. During summer, higher and more frequent precipitations (lower probability of long dry sequences and lower return period of 15 days and severity) were presented whereas the opposite was found in winter. However, the stations located to the west presented the highest probability of long dry sequences with higher severity and lower accumulated precipitation. This result highlights the vulnerability of the agriculture activity in the western stations. Regarding the impact of long dry sequences over soil water storage, the seasonality of evapotranspiration is also involved. The impact is stronger during austral summer because of higher values of evapotranspiration and it is lower during winter, in spite of the higher probability of long sequences. Decadal analysis suggested that soil water storage responds to precipitation amount or frequency depending on the magnitude of the anomalies. In this sense, the impact of precipitation over soil water storage depends on how it is distributed.
Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. In this research, long dry spells (longer than 15 days) and their impact on soil water storage were analysed in the eastern region of rain‐fed agriculture production of Argentina. The results highlight the vulnerability of the agriculture activity in the western stations and the role of evapotranspiration which enhances the effects of long dry spells in certain seasons.</description><identifier>ISSN: 0899-8418</identifier><identifier>EISSN: 1097-0088</identifier><identifier>DOI: 10.1002/joc.5087</identifier><language>eng</language><publisher>Chichester, UK: John Wiley & Sons, Ltd</publisher><subject>Agricultural production ; Agriculture ; Anomalies ; Atmospheric precipitations ; Dry spells ; Economic impact ; Evapotranspiration ; Extreme weather ; Impact analysis ; Moisture content ; Precipitation ; precipitation distribution ; Probability theory ; Rain ; Rainfall ; Regional development ; return period ; Seasonal variations ; Seasonality ; Soil ; Soil analysis ; Soil water ; Soil water storage ; soil‐atmosphere interaction ; Spatial distribution ; Spatial variability ; Spatial variations ; Stations ; Storage ; Summer ; Vulnerability ; Water ; Water storage ; Weather ; Weather conditions ; Winter</subject><ispartof>International journal of climatology, 2017-10, Vol.37 (12), p.4316-4326</ispartof><rights>2017 Royal Meteorological Society</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3507-c2d470e0c582513b915d34cf4a830be38b9ef59547e978d8a8ff33bf7ad801483</citedby><cites>FETCH-LOGICAL-a3507-c2d470e0c582513b915d34cf4a830be38b9ef59547e978d8a8ff33bf7ad801483</cites><orcidid>0000-0002-0287-7522</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fjoc.5087$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fjoc.5087$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27923,27924,45573,45574</link.rule.ids></links><search><creatorcontrib>Pántano, Vanesa C.</creatorcontrib><creatorcontrib>Penalba, Olga C.</creatorcontrib><creatorcontrib>Spescha, Liliana B.</creatorcontrib><creatorcontrib>Murphy, Guillermo M.</creatorcontrib><title>Assessing how accumulated precipitation and long dry sequences impact the soil water storage</title><title>International journal of climatology</title><description>ABSTRACT
Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. The temporal and spatial variability of these variables, together with the evapotranspiration, is crucial in the east‐northeast of Argentina, where rain‐fed agricultural production is carried out. In this work, the frequency of precipitation was studied from dry spells and complemented with an analysis of the accumulated precipitation and evapotranspiration. In particular, dry sequences longer than 15 days, return period and severity, were the focus of this study. Finally, the impact of the amount and frequency of precipitation on soil water storage was assessed through a decadal analysis. The region of study is characterized by northeast‐southwest gradient in accumulated precipitation and east–west gradient in winter long dry sequences. During summer, higher and more frequent precipitations (lower probability of long dry sequences and lower return period of 15 days and severity) were presented whereas the opposite was found in winter. However, the stations located to the west presented the highest probability of long dry sequences with higher severity and lower accumulated precipitation. This result highlights the vulnerability of the agriculture activity in the western stations. Regarding the impact of long dry sequences over soil water storage, the seasonality of evapotranspiration is also involved. The impact is stronger during austral summer because of higher values of evapotranspiration and it is lower during winter, in spite of the higher probability of long sequences. Decadal analysis suggested that soil water storage responds to precipitation amount or frequency depending on the magnitude of the anomalies. In this sense, the impact of precipitation over soil water storage depends on how it is distributed.
Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. In this research, long dry spells (longer than 15 days) and their impact on soil water storage were analysed in the eastern region of rain‐fed agriculture production of Argentina. The results highlight the vulnerability of the agriculture activity in the western stations and the role of evapotranspiration which enhances the effects of long dry spells in certain seasons.</description><subject>Agricultural production</subject><subject>Agriculture</subject><subject>Anomalies</subject><subject>Atmospheric precipitations</subject><subject>Dry spells</subject><subject>Economic impact</subject><subject>Evapotranspiration</subject><subject>Extreme weather</subject><subject>Impact analysis</subject><subject>Moisture content</subject><subject>Precipitation</subject><subject>precipitation distribution</subject><subject>Probability theory</subject><subject>Rain</subject><subject>Rainfall</subject><subject>Regional development</subject><subject>return period</subject><subject>Seasonal variations</subject><subject>Seasonality</subject><subject>Soil</subject><subject>Soil analysis</subject><subject>Soil water</subject><subject>Soil water storage</subject><subject>soil‐atmosphere interaction</subject><subject>Spatial distribution</subject><subject>Spatial variability</subject><subject>Spatial variations</subject><subject>Stations</subject><subject>Storage</subject><subject>Summer</subject><subject>Vulnerability</subject><subject>Water</subject><subject>Water storage</subject><subject>Weather</subject><subject>Weather conditions</subject><subject>Winter</subject><issn>0899-8418</issn><issn>1097-0088</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp10D1PwzAQBmALgUQpSPwESywsKefaxuexqvhUpS6wIUWO47Su0jjYiaL-e1LKynTL896dXkJuGcwYwPxhF-xMAqozMmGgVQaAeE4mgFpnKBhekquUdgCgNXuckK9FSi4l32zoNgzUWNvv-9p0rqRtdNa3vjOdDw01TUnrMLIyHmhy371rrEvU71tjO9ptHU3B13QYo5GmLkSzcdfkojJ1cjd_c0o-n58-lq_Zav3ytlysMsMlqMzOS6HAgZU4l4wXmsmSC1sJgxwKx7HQrpJaCuW0whINVhXnRaVMicAE8im5O-1tYxgfS12-C31sxpM500JoyRmqUd2flI0hpeiqvI1-b-IhZ5AfuxtTNj92N9LsRAdfu8O_Ln9fL3_9D5NHcKI</recordid><startdate>201710</startdate><enddate>201710</enddate><creator>Pántano, Vanesa C.</creator><creator>Penalba, Olga C.</creator><creator>Spescha, Liliana B.</creator><creator>Murphy, Guillermo M.</creator><general>John Wiley & Sons, Ltd</general><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0002-0287-7522</orcidid></search><sort><creationdate>201710</creationdate><title>Assessing how accumulated precipitation and long dry sequences impact the soil water storage</title><author>Pántano, Vanesa C. ; Penalba, Olga C. ; Spescha, Liliana B. ; Murphy, Guillermo M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3507-c2d470e0c582513b915d34cf4a830be38b9ef59547e978d8a8ff33bf7ad801483</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Agricultural production</topic><topic>Agriculture</topic><topic>Anomalies</topic><topic>Atmospheric precipitations</topic><topic>Dry spells</topic><topic>Economic impact</topic><topic>Evapotranspiration</topic><topic>Extreme weather</topic><topic>Impact analysis</topic><topic>Moisture content</topic><topic>Precipitation</topic><topic>precipitation distribution</topic><topic>Probability theory</topic><topic>Rain</topic><topic>Rainfall</topic><topic>Regional development</topic><topic>return period</topic><topic>Seasonal variations</topic><topic>Seasonality</topic><topic>Soil</topic><topic>Soil analysis</topic><topic>Soil water</topic><topic>Soil water storage</topic><topic>soil‐atmosphere interaction</topic><topic>Spatial distribution</topic><topic>Spatial variability</topic><topic>Spatial variations</topic><topic>Stations</topic><topic>Storage</topic><topic>Summer</topic><topic>Vulnerability</topic><topic>Water</topic><topic>Water storage</topic><topic>Weather</topic><topic>Weather conditions</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pántano, Vanesa C.</creatorcontrib><creatorcontrib>Penalba, Olga C.</creatorcontrib><creatorcontrib>Spescha, Liliana B.</creatorcontrib><creatorcontrib>Murphy, Guillermo M.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>International journal of climatology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pántano, Vanesa C.</au><au>Penalba, Olga C.</au><au>Spescha, Liliana B.</au><au>Murphy, Guillermo M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Assessing how accumulated precipitation and long dry sequences impact the soil water storage</atitle><jtitle>International journal of climatology</jtitle><date>2017-10</date><risdate>2017</risdate><volume>37</volume><issue>12</issue><spage>4316</spage><epage>4326</epage><pages>4316-4326</pages><issn>0899-8418</issn><eissn>1097-0088</eissn><abstract>ABSTRACT
Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. The temporal and spatial variability of these variables, together with the evapotranspiration, is crucial in the east‐northeast of Argentina, where rain‐fed agricultural production is carried out. In this work, the frequency of precipitation was studied from dry spells and complemented with an analysis of the accumulated precipitation and evapotranspiration. In particular, dry sequences longer than 15 days, return period and severity, were the focus of this study. Finally, the impact of the amount and frequency of precipitation on soil water storage was assessed through a decadal analysis. The region of study is characterized by northeast‐southwest gradient in accumulated precipitation and east–west gradient in winter long dry sequences. During summer, higher and more frequent precipitations (lower probability of long dry sequences and lower return period of 15 days and severity) were presented whereas the opposite was found in winter. However, the stations located to the west presented the highest probability of long dry sequences with higher severity and lower accumulated precipitation. This result highlights the vulnerability of the agriculture activity in the western stations. Regarding the impact of long dry sequences over soil water storage, the seasonality of evapotranspiration is also involved. The impact is stronger during austral summer because of higher values of evapotranspiration and it is lower during winter, in spite of the higher probability of long sequences. Decadal analysis suggested that soil water storage responds to precipitation amount or frequency depending on the magnitude of the anomalies. In this sense, the impact of precipitation over soil water storage depends on how it is distributed.
Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. In this research, long dry spells (longer than 15 days) and their impact on soil water storage were analysed in the eastern region of rain‐fed agriculture production of Argentina. The results highlight the vulnerability of the agriculture activity in the western stations and the role of evapotranspiration which enhances the effects of long dry spells in certain seasons.</abstract><cop>Chichester, UK</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/joc.5087</doi><tpages>11</tpages><orcidid>https://orcid.org/0000-0002-0287-7522</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Agricultural production Agriculture Anomalies Atmospheric precipitations Dry spells Economic impact Evapotranspiration Extreme weather Impact analysis Moisture content Precipitation precipitation distribution Probability theory Rain Rainfall Regional development return period Seasonal variations Seasonality Soil Soil analysis Soil water Soil water storage soil‐atmosphere interaction Spatial distribution Spatial variability Spatial variations Stations Storage Summer Vulnerability Water Water storage Weather Weather conditions Winter |
title | Assessing how accumulated precipitation and long dry sequences impact the soil water storage |
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