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Sökning: onr:"swepub:oai:DiVA.org:su-161213" > Effects of Hydrocli...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00004114naa a2200565 4500
001oai:DiVA.org:su-161213
003SwePub
008181025s2018 | |||||||||||000 ||eng|
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1612132 URI
0247 a https://doi.org/10.1007/s13157-018-1024-72 DOI
040 a (SwePub)su
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
1001 a Jaramillo, Fernandou Stockholms universitet,Institutionen för naturgeografi,Stockholm Resilience Centre,Florida International University, USA4 aut0 (Swepub:su)fjara
2451 0a Effects of Hydroclimatic Change and Rehabilitation Activities on Salinity and Mangroves in the Cienaga Grande de Santa Marta, Colombia
264 c 2018-03-30
264 1b Springer Science and Business Media LLC,c 2018
338 a print2 rdacarrier
520 a The Cienaga Grande de Santa Marta (CGSM), Colombia is possibly the wetland that has experienced the largest mangrove mortality on record due to modification of hydrologic connectivity and consequent hypersaline conditions. We used hydroclimatic, salinity and mangrove basal area data collected in five stations from 1993 to 2015 to study the relation between ongoing mangrove recovery, changes in salinity in the wetland and hydroclimatic changes in precipitation, potential evapotranspiration and freshwater inputs. We found that until 2015, the mangrove ecosystems in CGSM are in general terms in a path of recovery due to the combined effect of favorable hydroclimatic conditions and management operations to increase freshwater inputs into the wetland. We observed in three stations that the annual growth of mangrove basal area increased as pore water salinity decreased. Regarding surface water salinity, El Nino/Southern Oscillation explained most of the inter-annual variability in the wet season by regulating freshwater and in the dry season by regulating potential evaporation from the wetland. However, persistent channel reopening appeared to be the cause for the largest salinity decreases, whereas lack of persistent dredging slowed recovery in other areas. The monitoring of the mangrove-salinity-hydroclimate system must continue in order to increase its understanding and to avoid more recurring episodes of mangrove mortality.
650 7a NATURVETENSKAPx Biologi0 (SwePub)1062 hsv//swe
650 7a NATURAL SCIENCESx Biological Sciences0 (SwePub)1062 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653 a Mangroves
653 a Mortality
653 a Recovery
653 a Salinity
653 a Hydroclimate
653 a Wetland connectivity
653 a Freshwater inputs
653 a Channel reopening
7001 a Licero, Lucia4 aut
7001 a Åhlen, Imenneu Stockholms universitet,Institutionen för naturgeografi4 aut0 (Swepub:su)imbe1931
7001 a Manzoni, Stefanou Stockholms universitet,Institutionen för naturgeografi4 aut0 (Swepub:su)smanz
7001 a Alexandra Rodriguez-Rodriguez, Jenny4 aut
7001 a Guittard, Aliceu Stockholms universitet,Institutionen för naturgeografi4 aut
7001 a Hylin, Annau Stockholms universitet,Institutionen för naturgeografi4 aut
7001 a Bolanos, Jiner4 aut
7001 a Jawitz, James4 aut
7001 a Wdowinski, Shimon4 aut
7001 a Martinez, Oscar4 aut
7001 a Fernanda Espinosa, Luisa4 aut
7102 a Stockholms universitetb Institutionen för naturgeografi4 org
7730 t Wetlands (Wilmington, N.C.)d : Springer Science and Business Media LLCg 38:4, s. 755-767q 38:4<755-767x 0277-5212x 1943-6246
8564 u https://doi.org/10.1007/s13157-018-1024-7y Fulltext
8564 u https://link.springer.com/content/pdf/10.1007%2Fs13157-018-1024-7.pdf
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-161213
8564 8u https://doi.org/10.1007/s13157-018-1024-7

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