Global warming and the future of Caribbean coral reefs
Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, the...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Graus, Richard R. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1998 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© The Northeasten Science Foundation, Inc 1998 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Carbonates and evaporites - Springer Netherlands, 1986, 13(1998), 1 vom: 01. März, Seite 43-47 |
|---|---|
| Übergeordnetes Werk: |
volume:13 ; year:1998 ; number:1 ; day:01 ; month:03 ; pages:43-47 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF03175433 |
|---|
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OLC2076497854 |
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| 520 | |a Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, these reefs will gradually become more submerged. As they deepen, higher waves will propagate into back-reef areas, altering the ecological and sedimentological zonation patterns and accelerating the erosion of leeward shelves and shores. Resuspended sediment will increase the turbidity, causing the demise of sediment-sensitive corals and possibly entire reef communities. | ||
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10.1007/BF03175433 doi (DE-627)OLC2076497854 (DE-He213)BF03175433-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Graus, Richard R. verfasserin aut Global warming and the future of Caribbean coral reefs 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Northeasten Science Foundation, Inc 1998 Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, these reefs will gradually become more submerged. As they deepen, higher waves will propagate into back-reef areas, altering the ecological and sedimentological zonation patterns and accelerating the erosion of leeward shelves and shores. Resuspended sediment will increase the turbidity, causing the demise of sediment-sensitive corals and possibly entire reef communities. Coral Reef Fore Reef Reef Crest Caribbean Reef Caribbean Coral Reef Macintyre, Ian G. aut Enthalten in Carbonates and evaporites Springer Netherlands, 1986 13(1998), 1 vom: 01. März, Seite 43-47 (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:13 year:1998 number:1 day:01 month:03 pages:43-47 https://doi.org/10.1007/BF03175433 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_69 GBV_ILN_381 GBV_ILN_4309 AR 13 1998 1 01 03 43-47 |
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10.1007/BF03175433 doi (DE-627)OLC2076497854 (DE-He213)BF03175433-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Graus, Richard R. verfasserin aut Global warming and the future of Caribbean coral reefs 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Northeasten Science Foundation, Inc 1998 Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, these reefs will gradually become more submerged. As they deepen, higher waves will propagate into back-reef areas, altering the ecological and sedimentological zonation patterns and accelerating the erosion of leeward shelves and shores. Resuspended sediment will increase the turbidity, causing the demise of sediment-sensitive corals and possibly entire reef communities. Coral Reef Fore Reef Reef Crest Caribbean Reef Caribbean Coral Reef Macintyre, Ian G. aut Enthalten in Carbonates and evaporites Springer Netherlands, 1986 13(1998), 1 vom: 01. März, Seite 43-47 (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:13 year:1998 number:1 day:01 month:03 pages:43-47 https://doi.org/10.1007/BF03175433 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_69 GBV_ILN_381 GBV_ILN_4309 AR 13 1998 1 01 03 43-47 |
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10.1007/BF03175433 doi (DE-627)OLC2076497854 (DE-He213)BF03175433-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Graus, Richard R. verfasserin aut Global warming and the future of Caribbean coral reefs 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Northeasten Science Foundation, Inc 1998 Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, these reefs will gradually become more submerged. As they deepen, higher waves will propagate into back-reef areas, altering the ecological and sedimentological zonation patterns and accelerating the erosion of leeward shelves and shores. Resuspended sediment will increase the turbidity, causing the demise of sediment-sensitive corals and possibly entire reef communities. Coral Reef Fore Reef Reef Crest Caribbean Reef Caribbean Coral Reef Macintyre, Ian G. aut Enthalten in Carbonates and evaporites Springer Netherlands, 1986 13(1998), 1 vom: 01. März, Seite 43-47 (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:13 year:1998 number:1 day:01 month:03 pages:43-47 https://doi.org/10.1007/BF03175433 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_69 GBV_ILN_381 GBV_ILN_4309 AR 13 1998 1 01 03 43-47 |
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10.1007/BF03175433 doi (DE-627)OLC2076497854 (DE-He213)BF03175433-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Graus, Richard R. verfasserin aut Global warming and the future of Caribbean coral reefs 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Northeasten Science Foundation, Inc 1998 Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, these reefs will gradually become more submerged. As they deepen, higher waves will propagate into back-reef areas, altering the ecological and sedimentological zonation patterns and accelerating the erosion of leeward shelves and shores. Resuspended sediment will increase the turbidity, causing the demise of sediment-sensitive corals and possibly entire reef communities. Coral Reef Fore Reef Reef Crest Caribbean Reef Caribbean Coral Reef Macintyre, Ian G. aut Enthalten in Carbonates and evaporites Springer Netherlands, 1986 13(1998), 1 vom: 01. März, Seite 43-47 (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:13 year:1998 number:1 day:01 month:03 pages:43-47 https://doi.org/10.1007/BF03175433 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_69 GBV_ILN_381 GBV_ILN_4309 AR 13 1998 1 01 03 43-47 |
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Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, these reefs will gradually become more submerged. As they deepen, higher waves will propagate into back-reef areas, altering the ecological and sedimentological zonation patterns and accelerating the erosion of leeward shelves and shores. Resuspended sediment will increase the turbidity, causing the demise of sediment-sensitive corals and possibly entire reef communities. © The Northeasten Science Foundation, Inc 1998 |
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Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, these reefs will gradually become more submerged. As they deepen, higher waves will propagate into back-reef areas, altering the ecological and sedimentological zonation patterns and accelerating the erosion of leeward shelves and shores. Resuspended sediment will increase the turbidity, causing the demise of sediment-sensitive corals and possibly entire reef communities. © The Northeasten Science Foundation, Inc 1998 |
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Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, these reefs will gradually become more submerged. As they deepen, higher waves will propagate into back-reef areas, altering the ecological and sedimentological zonation patterns and accelerating the erosion of leeward shelves and shores. Resuspended sediment will increase the turbidity, causing the demise of sediment-sensitive corals and possibly entire reef communities. © The Northeasten Science Foundation, Inc 1998 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2076497854</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230401175233.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s1998 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF03175433</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2076497854</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF03175433-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Graus, Richard R.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Global warming and the future of Caribbean coral reefs</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1998</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Northeasten Science Foundation, Inc 1998</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Computer simulations with the COREEF model (Graus et al. 1984) demonstrate that the growth of Caribbean coral reefs will be unable to match all but the most optimistic predicted rates of sea level rise that global warming is expected to cause over the next few centuries, and, therefore, these reefs will gradually become more submerged. 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