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Granato-Souza - Rio Paru - CEOD - ITRDB BRA011

Originator:

Granato-Souza, D.; Pereira, G.A.; Barbosa, A.C.

Citation Information:

Zuidema, P.A., F. Babst, P. Groenendijk, V. Trouet, A. Abiyu, R. Acuña-Soto, E. Adenesky-Filho, R. Alfaro-Sánchez, J.R. Vieira Aragão, G. Assis-Pereira, X. Bai, A.C. Barbosa, G. Battipaglia, H. Beeckman, P.C. Botosso, T. Bradley, A. Bräuning, R. Brienen, B.M. Buckley, J.J. Camarero, A. Carvalho, G. Ceccantini, L.R. Centeno-Erguera, J. Cerano-Paredes, Á.A. Chávez-Durán, B.B.L. Cintra, M.K. Cleaveland, C. Couralet, R. D'Arrigo, J.I. Del Valle, O. Dünisch, B.J. Enquist, K. Esemann-Quadros, Z. Eshetu, Z.-X. Fan, M.E. Ferrero, E. Fichtler, C. Fontana, K.S. Francisco, A. Gebrekirstos, E. Gloor, D. Granato-Souza, K. Haneca, G.L. Harley, I. Heinrich, G. Helle, J.G. Inga, M. Islam, Y.-M. Jiang, M. Kaib, Z.H. Khamisi, M. Koprowski, B. Kruijt, E. Layme, R. Leemans, A.J. Leffler, C.S. Lisi, N.J. Loader, G.M. Locosselli, L. Lopez, M.I. López-Hernández, J.L.P.C. Lousada, H.A. Mendivelso, M. Mokria, V. Ribeiro Montóia, E. Moors, C. Nabais, J. Ngoma, F.d.C. Nogueira Júnior, J.M. Oliveira, G.M. Olmedo, M.A. Pagotto, S. Panthi, G. Pérez-De-Lis, D. Pucha-Cofrep, N. Pumijumnong, M. Rahman, J.A. Ramirez, E.J. Requena-Rojas, A.d.S. Ribeiro, I. Robertson, F.A. Roig, E.A. Rubio-Camacho, U. Sass-Klaassen, J. Schöngart, P.R. Sheppard, F. Slotta, J.H. Speer, M.D. Therrell, B. Toirambe, M. Tomazello-Filho, M.C.A. Torbenson, R. Touchan, A. Venegas-González, R. Villalba, J. Villanueva-Diaz, R. Vinya, M. Vlam, T. Wils, Z.-K. Zhou. 2022. Tropical tree growth driven by dry-season climate variability. Nature Geoscience, 15, 269–276. doi: 10.1038/s41561-022-00911-8

Lat:0, Lon:0

Download Data:

Rio Paru
Correlation Stats	bra011.txt
Raw Measurements	bra011.rwl
Raw Measurements - NOAA Template File	bra011-rwl-noaa.txt

Use Constraints:

Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.

Distributor:

National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce

Resource Description (data set id):

noaa-tree-36018

Data Coverage:

Latitude: -0.97669
Longitude: -53.32586
Minimum Elevation: 163 m
Maximum Elevation: 163 m
Earliest Year: 164 cal yr BP (1786 CE)
Most Recent Year: -66 cal yr BP (2016 CE)

Science Keywords:

Spanish cedar
CEOD
Cedrela odorata L.

Tree Species:

CEOD (Cedrela odorata L.)
Spanish cedar

Parameters:

earth science>paleoclimate>tree-ring>width

Variables:

what	unit	info
age	year Common Era
total ring width	millimeter	Tree ID: PAR11C;
total ring width	millimeter	Tree ID: PAR01A;
total ring width	millimeter	Tree ID: PAR01B;
total ring width	millimeter	Tree ID: PAR01C;
total ring width	millimeter	Tree ID: PAR03A;
total ring width	millimeter	Tree ID: PAR03B;
total ring width	millimeter	Tree ID: PAR03C;
total ring width	millimeter	Tree ID: PAR04A;
total ring width	millimeter	Tree ID: PAR04B;
total ring width	millimeter	Tree ID: PAR04C;
total ring width	millimeter	Tree ID: PAR06A;
total ring width	millimeter	Tree ID: PAR06B;
total ring width	millimeter	Tree ID: PAR06C;
total ring width	millimeter	Tree ID: PAR07A;
total ring width	millimeter	Tree ID: PAR07B;
total ring width	millimeter	Tree ID: PAR07C;
total ring width	millimeter	Tree ID: PAR08A;
total ring width	millimeter	Tree ID: PAR08B;
total ring width	millimeter	Tree ID: PAR11A;
total ring width	millimeter	Tree ID: PAR11B;
total ring width	millimeter	Tree ID: PAR13A;
total ring width	millimeter	Tree ID: PAR13B;
total ring width	millimeter	Tree ID: PAR17A;
total ring width	millimeter	Tree ID: PAR17B;
total ring width	millimeter	Tree ID: PAR19A;
total ring width	millimeter	Tree ID: PAR19B;
total ring width	millimeter	Tree ID: PAR22A;
total ring width	millimeter	Tree ID: PAR22B;
total ring width	millimeter	Tree ID: PAR27A;
total ring width	millimeter	Tree ID: PAR27B;
total ring width	millimeter	Tree ID: PAR28A;
total ring width	millimeter	Tree ID: PAR28B;
total ring width	millimeter	Tree ID: PAR28C;
total ring width	millimeter	Tree ID: PAR29A;
total ring width	millimeter	Tree ID: PAR29B;
total ring width	millimeter	Tree ID: PAR30A;
total ring width	millimeter	Tree ID: PAR30B;
total ring width	millimeter	Tree ID: PAR30C;
total ring width	millimeter	Tree ID: PAR31A;
total ring width	millimeter	Tree ID: PAR31B;
total ring width	millimeter	Tree ID: PAR33B;
total ring width	millimeter	Tree ID: PAR36A;
total ring width	millimeter	Tree ID: PAR36B;
total ring width	millimeter	Tree ID: PAR41A;
total ring width	millimeter	Tree ID: PAR41B;
total ring width	millimeter	Tree ID: PAR42A;
total ring width	millimeter	Tree ID: PAR42B;
total ring width	millimeter	Tree ID: PAR43A;
total ring width	millimeter	Tree ID: PAR43B;
total ring width	millimeter	Tree ID: PAR44B;
total ring width	millimeter	Tree ID: PAR44C;
total ring width	millimeter	Tree ID: PAR45A;
total ring width	millimeter	Tree ID: PAR45B;
total ring width	millimeter	Tree ID: PAR45C;
total ring width	millimeter	Tree ID: PAR47A;
total ring width	millimeter	Tree ID: PAR47B;
total ring width	millimeter	units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999

Summary/Abstract:

Interannual variability in the global land carbon sink is strongly related to variations in tropical temperature and rainfall. This association suggests an important role for moisture-driven fluctuations in tropical vegetation productivity, but empirical evidence to quantify the responsible ecological processes is missing. Such evidence can be obtained from tree-ring data that quantify variability in a major vegetation productivity component: woody biomass growth. Here we compile a pantropical tree-ring network to show that annual woody biomass growth increases primarily with dry-season precipitation and decreases with dry-season maximum temperature. The strength of these dry-season climate responses varies among sites, as reflected in four robust and distinct climate response groups of tropical tree growth derived from clustering. Using cluster and regression analyses, we find that dry-season climate responses are amplified in regions that are drier, hotter and more climatically variable. These amplification patterns suggest that projected global warming will probably aggravate drought-induced declines in annual tropical vegetation productivity. Our study reveals a previously underappreciated role of dry-season climate variability in driving the dynamics of tropical vegetation productivity and consequently in influencing the land carbon sink.

Study Notes:

NOAA Template Raw Measurements file added 2022-04-04.

More Information:

TREE RING

Contact Information:

DOC/NOAA/NESDIS/NCEI

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USA

https://www.ncei.noaa.gov/products/paleoclimatology

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