23,850 research outputs found
Ambassador Mari-Luci Jaramillo arrival at airport in Tegucigalpa, Honduras
No full textFrom left to right, American Embassy Deputy, Ambassador Mari-Luci Jaramillo, protocol officer from Honduran Embassy, and Dr. H. J. Jaramillo walking away from the plane
JARAMILLO, J. Inés (Cap.)
No full textTelegrama del Cap. J. Inés Jaramillo al Gral. PEC. Solicita audiencia
Métricas de autor Alejandro Gómez Jaramillo
No full textInforme de las métricas de autor del Dr. Alejandro Gómez Jaramillo de las publicaciones indexadas en Google Académico cuyo objetivo es entregar un insumo para el fortalecimiento de las capacidades y potencialidades de los autores de la Universidad Santo Tomás en el posicionamiento y visibilidad de sus publicacionesReport of the author metrics Alejandro Gómez Jaramillo of the publications indexed in Google Scholar whose objective is to provide an input for the strengthening of the capacities and potentialities of the authors of the Santo Tomás University in the positioning and visibility of their publications.http://unidadinvestigacion.usta.edu.c
Temporal variability in the intertidal macroinfauna in the Queule river estuary, South-Central Chile
No full textPT: J; CR: ANDERSON FE, 1972, J SEDIMENT PETROL, V42, P602 ANDERSSON CA, 1981, ADV CERAM, V3, P184 BACHELET G, 1986, HYDROBIOLOGIA, V142, P233 BERTRAN C, 1984, STUDIES NEOTROPICAL, V19, P33 BERTRAN CE, 1989, REV CHIL HIST NAT, V62, P19 BRAVO A, 1984, MEDIO AMBIENTE CHILE, V7, P37 BRAVO A, 1989, THESIS U AUSTRAL CHI BUTMAN CA, 1987, OCEANOGR MAR BIOL, V25, P113 CHESTER AJ, 1983, B MAR SCI, V33, P282 DEWITT TH, 1985, J EXP MAR BIOL ECOL, V92, P97 DONOSO EP, 1991, THESIS U AUSTRAL CHI GRASSLE JF, 1974, J MARINE RE, V32, P253 HAIR JF, 1979, MULTIVARIATE ANAL HOLLAND AF, 1985, ESTUARIES, V8, P93 ISHIKAWA K, 1989, MAR BIOL, V102, P265 JARAMILLO E, 1984, PSZNI MAR ECOL, V5, P119 JARAMILLO E, 1985, REV CHIL HIST NAT, V58, P127 JARAMILLO E, 1985, STUDIES NEOTROPICAL, V20, P33 JENSEN KT, 1985, MAR ECOL-PROG SER, V25, P269 JENSEN KT, 1990, J EXP MAR BIOL ECOL, V137, P1 MEADOWS PS, 1989, MAR BIOL, V101, P75 NELSON WG, 1979, J EXP MAR BIOL ECOL, V39, P231 PETERSON C, 1984, J SEDIMENT PETROL, V4, P86 PETERSON CH, 1979, ECOLOGICAL PROCESSES, P233 PINO M, 1983, REV GEOLOGICA CHILE, V18, P77 RHOADS DC, 1982, ANIMAL SEDIMENT RELA, P3 RICHTER W, 1985, MAR BIOL, V86, P93 ROJAS C, 1983, INFORMATIVO GEOGRAFI, V31, P55 SOKAL RR, 1969, BIOMETRIA TUFAIL A, 1989, TOPICS MARINE BIOL, V53, P319 TURNER A, 1984, MEDIO AMBIENTE, V7, P29 TURNER A, 1988, THESIS U AUSTRAL CHI VANDOLAH RF, 1978, ECOL MONOGR, V48, P191 WILSON WH, 1988, OPHELIA, V29, P227 WILSON WH, 1990, ANNU REV ECOL SYST, V21, P221; NR: 35; TC: 13; J9: ESTUAR COAST SHELF SCI; PG: 13; GA: MQ162Source type: Electronic(1
Distribution and habitat structure of Ocypode gaudichaudii H. Milne Edwards & Lucas, 1843, in sandy beaches of Northern Chile
No full textTen sandy beaches along the coast of northern Chile (20-23 degreesS) were studied in December 1998, to examine the distribution, abundance, and habitat characteristics of the crab Ocypode gaudichaudii. Beach width. slope, and intertidal fringes were identified, and Dean's parameter, describing beach morphodynamic status, was calculated. Crabs were collected and burrows and physical characteristics of the burrow zones analysed. The burrow zone extended primarily across the dry and retention zones. Physical properties across the burrow areas did not influence burrow characteristics. Significant differences in burrow density were detected both within and among the 10 sandy beaches. These differences were not related to morphodynamic beach types, but could be explained by related aspects, such as the height of the drift line, and the width and slope of dry and retention zones. We linked these results to behavioural and not just to physical causes.PT: J; CR: DUGAN JE, 1991, J EXP MAR BIOL ECOL, V150, P63 DUGAN JE, 1996, REV CHIL HIST NAT, V69, P579 EMERY KO, 1938, J SEDIMENT PETROL, V8, P105 EMERY KO, 1961, LIMNOL OCEANOGR, V6, P90 JAMES RJ, 1996, ESTUAR COAST SHELF S, V43, P81 JARAMILLO E, 1987, VIE MILLIEU, V37, P165 JARAMILLO E, 1993, ESTUAR COAST SHELF S, V37, P615 JARAMILLO E, 1993, MAR ECOL-PROG SER, V101, P105 JARAMILLO E, 1998, REV CHIL HIST NAT, V71, P459 KOEPCKE H, 1953, CONTRIBUCION CONOCIM, V13, P9 KOEPCKE HW, 1952, PUBLICACION MUSEO NA, V8, P1 KURIHARA Y, 1989, MAR BIOL, V101, P153 LUCAS, 1843, CRUSTACEANA, V71, P47 MCARDLE SB, 1992, J COASTAL RES, V8, P398 MCLACHLAN A, 1980, J ZOOL, V15, P57 MCLACHLAN A, 1993, J COASTAL RES, V15, P27 MCLACHLAN A, 1995, J EXP MAR BIOL ECOL, V187, P147 MCLACHLAN A, 1995, OCEANOGR MAR BIOL, V33, P305 SEWARDTHOMPSON B, 1973, SEDIMENTOLOGY, V11, P83 SHOBER UM, 1993, MAR BIOL, V116, P53 SHORT AD, 1983, SANDY BEACHES ECOSYS, P133 SHUCHMAN E, 1978, MAR BIOL, V49, P255 SOKAL RR, 1994, BIOMETRY, P1 TROTT TJ, 1988, CRUSTACEANA, V55, P217 WADA K, 1993, MAR BIOL, V115, P47 WARBURG MR, 1979, MAR BEHAV PHYSL, V6, P147 WOLCOTT TG, 1978, J EXP MAR BIOL ECOL, V31, P67; NR: 27; TC: 3; J9: CRUSTACEANA; PN: Part 1; PG: 13; GA: 420GTSource type: Electronic(1
MDI active region evolution videos for BARD catalog
No full textCitation and Acknowledgements
Please cite both this database the paper describing it, as well as adding the following acknowledgement:
"The BARD catalog of BMRs was downloaded from the solar dynamo dataverse (https://dataverse.harvard.edu/dataverse/solardynamo), maintained by Andrés Muñoz-Jaramillo."
Database citation format is shown at the top of this page, underneath the database title. It can be downloaded in a variety of formats directly from this page
The papers describing this database are
S. Chatterjee, A. Munoz-Jaramillo, & D. Lamb. Human-efficient labeling of a solar flux emergence video dataset by a deep learning model, 27 May 2021, PREPRINT (Version 1) available at Research Square https://doi.org/10.21203/rs.3.rs-366908/v1
A. Munoz-Jaramillo, Z. A. Werginz, J. P. Vargas-Acosta, M. D. DeLuca, J. C. Windmueller, J. Zhang, D. W. Longcope, D. A. Lamb, C. E. DeForest, S. Vargas-Dominguez, J. W. Harvey, & P. C. H. Martens , IEEE International Conference on Big Data, 3194 (2016). https://ieeexplore.ieee.org/document/7840975
A. Munoz-Jaramillo, B. Navarrete, & L. A. Campusano , The Astrophysical Journal, Volume 920, Issue 1, id.31, 11 pp. https://ui.adsabs.harvard.edu/abs/2021ApJ...920...31M
Main Limitations
The main limitations of these data are:
Videos are assembled in a constant Carrington rotation frame so, BMRs may drift within the video due to differential rotation.
Many videos have gaps and thus, do not have a constant cadence. We addressed this by interpolating the missing frames. In these videos we do not include interpolated frames.
Description
The Active Region (AR) magnetic evolution videos are created by -
Projecting full-disc line-of-sight magnetograms into Carrington grid
Dividing the projected maps into 15 degrees x 15 degrees non-overlapping patches. Each patch is sampled into 90 pixels x 90 pixels resulting into pixel scale of (1/6) degree
Stacking a set of consecutive frames covering about half a solar rotation tied to each AR from Bipolar Active Region Detection (BARD) catalogue
A total of 2453 videos are available over the period 1996 - 2011 in 'fits' format. Within the 'fits' header-
'NAXIS1' represents number of x-pixels
'NAXIS2' represents number of y-pixels
'NAXIS3' represents number of frames
'TIMEXXXX' represents the time stamp for frame XXXX in YYYY-MM-DDTHH:MM:SS format
'CRVAL1' represents the starting Carrington Longitude (degrees) for each video
'CRVAL2' represents the starting Latitude (degrees) for each video
Each video is manually verified and a label of '0' or '1' is added to the name of video with '0' representing 'no new AR emergence within the video' and '1' representing 'AR emergence'
Relationships between community structure of the intertidal macroinfauna and sandy beach characteristics along the Chilean coast
No full textEight sandy beaches were seasonally sampled along the coast of Chile, from ca. 21 to 42degrees S (about 3000 km) to study the relationship between community structure 2 of the intertidal macroinfauna and beach characteristics. Sediment samples (0.1 m(2), 30 cm deep) were collected (July-September 1998 and December 1998-January 1999) with plastic cylinders at 15 equally spaced levels along three replicated transects extending from above the drift line to the swash zone. The sediment was sieved through a 1 mm mesh and the organisms collected stored in 5% formalin. To define beach types, Dean's parameter (0) was calculated from wave heights and periods, and fall velocity of sand particles from the swash zone. Crustaceans (mainly peracarids) were the most diverse group with 14 species, followed by polychaetes with 5 species. The talitrid amphipod Orchestoidea tuberculata, the cirolanid isopods Excirolana braziliensis and E. hirsuticauda and the anomuran decapod Emerita analoga were the most widely distributed and common species. Regression analyses between species richness, abundance and biomass of the whole macroinfauna versus sediment characteristics, beach face slopes and morphodynamic beach states showed no significant relationships. Thus, macroinfaunal community characteristics did not increase linearly from lower intermediate to higher intermediate or dissipative beach states as had been found before in Chile or in other coasts. A comparative analysis with data from sandy beaches of other world regions showed that the number of species inhabiting Chilean sandy beaches was generally lower, whereas total population abundances were generally higher compared with values reported elsewhere.PT: J; CR: ANSELL AD, 1972, MAR BIOL, V17, P38 BRAZEIRO A, 1996, ESTUARINE COASTAL SH, V21, P587 BROWER JE, 1977, FIELD LAB METHODS GE CROKER RA, 1975, CAN J ZOOL, V53, P42 DEFEO O, 2000, MAR ECOL-PROG SER, V212, P159 DERUYCK AMC, 1992, CAH BIOL MAR, V33, P147 DUGAN JE, 1996, REV CHIL HIST NAT, V69, P579 DUGAN JE, 2000, 5 CAL ISL S, P339 EMERY KO, 1938, J SEDIMENT PETROL, V8, P105 EMERY KO, 1961, LIMNOL OCEANOGR, V6, P90 ETTER RJ, 1992, NATURE, V360, P576 FOLK R, 1980, PETROLOGY SEDIMENTAR FONSECA T, 1987, INVEST PESQ, V34, P33 GIBBS RJ, 1971, J SEDIMENT PETROL, V41, P7 GOMEZ J, 1999, MAR ECOL-PROG SER, V182, P209 JARAMILLO E, 1987, THESIS U NEW HAMPSHI JARAMILLO E, 1993, ESTUAR COAST SHELF S, V37, P615 JARAMILLO E, 1996, REV CHIL HIST NAT, V69, P641 JARAMILLO E, 1998, REV CHIL HIST NAT, V71, P459 JARAMILLO E, 2000, REV CHIL HIST NAT, V73, P771 JARAMILLO E, 2001, ECOL STU AN, V151, P61 MCLACHLAN A, 1990, J COASTAL RES, V6, P57 MCLACHLAN A, 1993, J COASTAL RES, V15, P27 MCLACHLAN A, 1995, OCEANOGR MAR BIOL, V33, P305 MCLACHLAN A, 1996, REV CHIL HIST NAT, V69, P451 MCLACHLAN A, 1998, J COASTAL CONSERVATI, V4, P181 SEWARDTHOMPSON B, 1973, SEDIMENTOLOGY, V11, P83 SHORT AD, 1983, SANDY BEACHES ECOSYS, P133 SOKAL RR, 1995, BIOMETRY PRINCIPLES; NR: 29; TC: 11; J9: MAR ECOL-P S Z N I; PG: 20; GA: 509UHSource type: Electronic(1
Restricting open surjections
No full textWe show that any continuous open surjection from a complete metric space to another metric space can be restricted to a surjection for which the domain has the same density character as the target. This improves a recent result of Aron, Jaramillo and Le Donne
Escritura de liquidación de la sociedad Vásquez y J. Jaramillo de Guatemala
No full textEscritura de liquidación de la sociedad Vásquez y J. Jaramillo por muerte de los socios
Fotografía UDBC050421
No full textFotografía del ejemplar Duque-Jaramillo, J. 2139, determinado como Ouratea sp. en el año 202
- …
