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1

Bosio, Giulia, Elisa Malinverno, Igor Maria Villa, et al. "Tephrochronology and chronostratigraphy of the Miocene Chilcatay and Pisco formations (East Pisco Basin, Peru)." Newsletters on Stratigraphy 53, no. 2 (2020): 213–47. http://dx.doi.org/10.1127/nos/2019/0525.

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COLLARETA, Alberto, Olivier LAMBERT, Christian de MUIZON, PALOMINO Aldo Marcelo BENITES, Mario URBINA, and Giovanni BIANUCCI. "A new physeteroid from the late Miocene of Peru expands the diversity of extinct dwarf and pygmy sperm whales (Cetacea: Odontoceti: Kogiidae)." Comptes Rendus Palevol 19, no. 5 (2020): 79–100. https://doi.org/10.5852/cr-palevol2020v19a5.

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Nowadays, the odontocete family Kogiidae is monotypic and only includes two species of diminutive relatives of the great sperm whale <em>Physeter </em>Linnaeus, 1758. Conversely, a growing body of extinct species indicates that kogiids were diverse and disparate during the late Neogene. The fossil record of Kogiidae is, to date, represented by several cranial specimens from Mio-Pliocene localities of the Northern Hemisphere, with the significant Southern Hemisphere exception of the Pisco Formation of Peru, from which two genera were known so far, including <em>Scaphokogia </em>Muizon, 1988, a
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Uhen, Mark D., Nicholas D. Pyenson, Thomas J. Devries, Mario Urbina, and Paul R. Renne. "New Middle Eocene Whales from the Pisco Basin of Peru." Journal of Paleontology 85, no. 5 (2011): 955–69. http://dx.doi.org/10.1666/10-162.1.

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4

DeVries, Thomas J. "Early Paleogene brackish-water molluscs from the Caballas Formation of the East Pisco Basin (Southern Peru)." Journal of Natural History 53, no. 25 (2018): 1533–84. https://doi.org/10.1080/00222933.2018.1524032.

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DeVries, Thomas J. (2019): Early Paleogene brackish-water molluscs from the Caballas Formation of the East Pisco Basin (Southern Peru). Journal of Natural History 53 (25): 1533-1584, DOI: 10.1080/00222933.2018.1524032
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5

DeVries, T. J. "Oligocene deposition and Cenozoic sequence boundaries in the Pisco Basin (Peru)." Journal of South American Earth Sciences 11, no. 3 (1998): 217–31. http://dx.doi.org/10.1016/s0895-9811(98)00014-5.

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6

Steffen, Damian, Fritz Schlunegger, and Frank Preusser. "Drainage basin response to climate change in the Pisco valley, Peru." Geology 37, no. 6 (2009): 491–94. http://dx.doi.org/10.1130/g25475a.1.

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7

Collareta, Alberto, Olivier Lambert, Felix G. Marx, et al. "Vertebrate Palaeoecology of the Pisco Formation (Miocene, Peru): Glimpses into the Ancient Humboldt Current Ecosystem." Journal of Marine Science and Engineering 9, no. 11 (2021): 1188. http://dx.doi.org/10.3390/jmse9111188.

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The northward-flowing Humboldt Current hosts perpetually high levels of productivity along the western coast of South America. Here, we aim to elucidate the deep-time history of this globally important ecosystem based on a detailed palaeoecological analysis of the exceptionally preserved middle–upper Miocene vertebrate assemblages of the Pisco Formation of the East Pisco Basin, southern Peru. We summarise observations on hundreds of fossil whales, dolphins, seals, seabirds, turtles, crocodiles, sharks, rays, and bony fishes to reconstruct ecological relationships in the wake of the Middle Mioc
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8

Belia, Emilia R., and Kevin E. Nick. "Earliest Miocene calcareous nannofossil biostratigraphy from the low-latitude Pisco Basin (Peru)." Stratigraphy 16, no. 2 (2019): 87–105. http://dx.doi.org/10.29041/strat.16.2.87-105.

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9

Belia, Emilia R., Kevin E. Nick, Erika Bedoya Agudelo, and David K. Watkins. "Earliest Miocene calcareous nannofossil biostratigraphy from the low-latitude Pisco Basin (Peru)." Stratigraphy 16, no. 2 (2019): 87–105. http://dx.doi.org/10.29041/strat/16.2.87-105.

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10

Saldaña, Erick, Jennifer Alvarez, Jaime Laqui-Estaña, et al. "An Overview of 20 Years of Pisco Spirit Research: Trends and Gaps Revealed by a Systematic Review." Beverages 11, no. 3 (2025): 77. https://doi.org/10.3390/beverages11030077.

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Pisco is an emblematic spirit in Peru and Chile, made from fermented grapes, gaining growing scientific interest over the last two decades. This study aimed to map 20 years of research on Pisco through a systematic bibliometric review. A search was conducted in the Scopus database covering the period from 2004 to 2024, applying the Preferred Reporting Items for Systematic Reviews and Meta-Analyses (PRISMA) methodology for the transparent selection of scientific articles. The search strategy considered titles, abstracts, and keywords, using the terms “Pisco” and “schnapps”, excluding unrelated
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11

Zorrilla Marcos, Yulissa, Elizabeth Clotilde Panana Holgado, Jeiner Eloy Solorzano Poma, David Minaya Huerta, Luis Teodosio Javier Cabana, and Julio Cesar Coral Jamanca. "Generation of monthly mean flows using the Gr2m model for trend analysis." Universidad Ciencia y Tecnología 28, no. 124 (2024): 26–36. http://dx.doi.org/10.47460/uct.v28i124.841.

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This paper analyzes the monthly mean flow trend in the Chicama, Moche, and Santa basins. The research is framed in a descriptive and explanatory approach, with an experimental, longitudinal, and prospective design. The climatic data were collected using R software (version 3.6.3) from the gridded databases of precipitation (PISCO V2.0) and temperature (PISCO V1.0) developed by SENAMHI. Station locations were determined using specific geographic coordinates for each basin. This information served as an input variable for the flow simulation using the GR2M model. The simulated flows were used fo
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12

Lambert, Olivier, Alberto Collareta, Aldo Benites-Palomino, et al. "A new platyrostrine sperm whale from the Early Miocene of the southeastern Pacific (East Pisco Basin, Peru) supports affinities with the southwestern Atlantic cetacean fauna." Geodiversitas 45, no. 22 (2023): 659–79. https://doi.org/10.5252/geodiversitas2023v45a22.

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Lambert, Olivier, Collareta, Alberto, Benites-Palomino, Aldo, Merella, Marco, Muizon, Christian de, Bennion, Rebecca, Urbina, Mario, Bianucci, Giovanni (2023): A new platyrostrine sperm whale from the Early Miocene of the southeastern Pacific (East Pisco Basin, Peru) supports affinities with the southwestern Atlantic cetacean fauna. Geodiversitas 45 (22): 659-679, DOI: 10.5252/geodiversitas2023v45a22, URL: https://sciencepress.mnhn.fr/sites/default/files/articles/pdf/g2023v45a22.pdf
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13

Nobile, Francesco, Olivier Lambert, Giovanni Bianucci, et al. "Surviving a Dark Age: The Oldest Baleen-Bearing Whales (Cetacea: Chaeomysticeti) of Pacific South America (Lower Miocene, Peru)." Life 15, no. 3 (2025): 452. https://doi.org/10.3390/life15030452.

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The evolution of baleen whales (Mysticeti) comprises two main phases, namely, (i) a Paleogene phase, which saw the diversification of stem lineages, and (ii) a Neogene phase, dominated by modern-looking, toothless, baleen-bearing forms in the monophyletic group Chaeomysticeti. These two phases are separated by a global turnover event coinciding with a gap—or “dark age”—in the mysticete fossil record. This dark age occurred between 23 and ~18 Ma and is apparently detected worldwide, except in Zealandia. Here, we report on a new mysticete fossil from the Lower Miocene (Burdigalian: ~19.2 Ma) str
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14

BOSIO, Giulia, Valentina A. BRACCHI, Elisa MALINVERNO, et al. "Taphonomy of a Panopea Ménard de la Groye, 1807 shell bed from the Pisco Formation (Miocene, Peru)." Comptes Rendus Palevol 20, no. 8 (2021): 119–40. https://doi.org/10.5852/cr-palevol2021v20a8.

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Invertebrate taphonomy can provide significant information about the <em>post-mortem</em> processes that affected the fossil record. In the East Pisco Basin of southern Peru, a <em>Panopea</em> M&eacute;nard de la Groye, 1807 shell bed was found in the upper Miocene strata of the Pisco Formation, hinting at a peculiar biostratinomic and diagenetic history. This bed contains abundant invertebrate fossil molds cemented by dolomite. The specimens of the deep infaunal bivalve, <em>Panopea </em>sp.,<em> </em>occur together with bivalves representative of shallow infaunal species (<em>Trachycardium<
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15

Marx, Felix G., and Naoki Kohno. "A new Miocene baleen whale from the Peruvian desert." Royal Society Open Science 3, no. 10 (2016): 160542. http://dx.doi.org/10.1098/rsos.160542.

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The Pisco-Ica and Sacaco basins of southern Peru are renowned for their abundance of exceptionally preserved fossil cetaceans, several of which retain traces of soft tissue and occasionally even stomach contents. Previous work has mostly focused on odontocetes, with baleen whales currently being restricted to just three described taxa. Here, we report a new Late Miocene rorqual (family Balaenopteridae), Incakujira anillodefuego gen. et sp. nov., based on two exceptionally preserved specimens from the Pisco Formation exposed at Aguada de Lomas, Sacaco Basin, southern Peru. Incakujira overall cl
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16

Molina, Rubén Rojas, Gerardo Maghella Seminario, José Maguiña León, and Mirella Tejerina Caisan. "Contribution of Isotopic Techniques in the Hydrological Study of the Aquifers of Ica, Villacuri and Lanchas." Environmental Management and Sustainable Development 9, no. 2 (2020): 72. http://dx.doi.org/10.5296/emsd.v9i2.16954.

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Ica Aquifer located at the coastal zone of Ica River Valley, supplies 40% of the water to a number of farms of Ica Region which is one of the most productive valley of Peru that covers an area of 30,000 hectares of area, in which a diverse agricultural product are grown for local and external market. In the last 15 years, water-table of the aquifer was lowering at an elevated rate that concerned to farmers and authorities of the Peruvian Government, so a number of studies was carried out to increase the water supply to the agriculture areas.The main purpose of the study using isotope technique
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17

DeVries, Thomas J. "Early Paleogene brackish-water molluscs from the Caballas Formation of the East Pisco Basin (Southern Peru)." Journal of Natural History 53, no. 25-26 (2018): 1533–84. http://dx.doi.org/10.1080/00222933.2018.1524032.

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18

Collareta, Alberto, Rafael Varas-Malca, Giulia Bosio, Mario Urbina, and Giovanni Coletti. "Ghosts of the Holobiont: Borings on a Miocene Turtle Carapace from the Pisco Formation (Peru) as Witnesses of Ancient Symbiosis." Journal of Marine Science and Engineering 11, no. 1 (2022): 45. http://dx.doi.org/10.3390/jmse11010045.

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In spite of the widespread occurrence of epibiotic turtle barnacles (Coronuloidea: Chelonibiidae and Platylepadidae) on extant marine turtles (Chelonioidea: Cheloniidae and Dermochelyidae), and although the association between these cirripedes and their chelonian hosts has existed for more than 30 million years, only a few studies have investigated the deep past of this iconic symbiotic relationship on palaeontological grounds. We describe probable platylepadid attachment scars in the form of hemispherical/hemiellipsoidal borings on an Upper Miocene (Tortonian) fragmentary turtle carapace, ide
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19

Bosio, Giulia, Elisa Malinverno, Alberto Collareta, et al. "Strontium Isotope Stratigraphy and the thermophilic fossil fauna from the middle Miocene of the East Pisco Basin (Peru)." Journal of South American Earth Sciences 97 (January 2020): 102399. http://dx.doi.org/10.1016/j.jsames.2019.102399.

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20

Di Celma, C., E. Malinverno, A. Collareta, et al. "Facies analysis, stratigraphy and marine vertebrate assemblage of the lower Miocene Chilcatay Formation at Ullujaya (Pisco basin, Peru)." Journal of Maps 14, no. 2 (2018): 257–68. http://dx.doi.org/10.1080/17445647.2018.1456490.

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21

Di Celma, C., P. P. Pierantoni, E. Malinverno, et al. "Allostratigraphy and paleontology of the lower Miocene Chilcatay Formation in the Zamaca area, East Pisco basin, southern Peru." Journal of Maps 15, no. 2 (2019): 393–405. http://dx.doi.org/10.1080/17445647.2019.1604439.

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22

Alvarez Villanueva, Jairo Isaí, and José Francisco Huamán Vidaurre. "Aplicación de hidrogramas unitarios mediante el producto PISCO (Peruvian Interpolated data of SENAMHI's Climatological and Hydrological Observations) para la generación de caudales máximos." Manglar 22, no. 1 (2025): 112–22. https://doi.org/10.57188/manglar.2025.013.

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The objective was to apply Unit Hydrographs using the PISCO product (Peruvian Interpolated data of SENAMHI's Climatological and Hydrological Observations) for the generation of maximum flows. Information was available on maximum monthly flows from the "Yonán" hydrometric station on the Jequetepeque River, with maximum monthly precipitation from 8 terrestrial stations in the upper Jequetepeque basin and maximum monthly precipitation from previously mentioned gridded spatial rainfall data for the period 1981-2019. The SCS Triangular Unit Hydrograph model and Snyder Synthetic Unit Hydrograph were
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23

ROQUE QUIROZ, RUBEN ANTHONY. "Validación de la data de precipitación (1981-2016) del producto PISCO v2.1: Estación meteorológica, elevación, estacionalidad del año y región climática en la cuenca Tumbes, Perú." Manglar 20, no. 1 (2023): 41–50. http://dx.doi.org/10.57188/manglar.2023.005.

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The scarce information that is counted and its importance in hydrological studies helps us to understand, simulate, and predict the events associated with the behavior of water. I think it is necessary to check the gridded data PISCOpm V.2.1 monthly rainfall with the observations in our Tumbes basin. For this, a comparative study was carried out between the observed and estimated values, concerning the weather station, elevation, seasonality of the year, and climatic region. Indicators such as the Coefficient of Determination(R2), Nash-Sutcliffe Efficiency Index (NS), and Percentage Statistica
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Rustichelli, Andrea, Claudio Di Celma, Emanuele Tondi, and Giovanni Bianucci. "Deformation within the Pisco Basin sedimentary record (southern Peru): Stratabound orthogonal vein sets and their impact on fault development." Journal of South American Earth Sciences 65 (January 2016): 79–100. http://dx.doi.org/10.1016/j.jsames.2015.11.002.

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25

Lambert, Olivier, Christian de Muizon, Mario Urbina, and Giovanni Bianucci. "A new longirostrine sperm whale (Cetacea, Physeteroidea) from the lower Miocene of the Pisco Basin (southern coast of Peru)." Journal of Systematic Palaeontology 18, no. 20 (2020): 1707–42. http://dx.doi.org/10.1080/14772019.2020.1805520.

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26

Bianucci, Giovanni, Alberto Collareta, Giulia Bosio, et al. "Taphonomy and palaeoecology of the lower Miocene marine vertebrate assemblage of Ullujaya (Chilcatay Formation, East Pisco Basin, southern Peru)." Palaeogeography, Palaeoclimatology, Palaeoecology 511 (December 2018): 256–79. http://dx.doi.org/10.1016/j.palaeo.2018.08.013.

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27

DeVries, Thomas J., John A. Barron, Diana Ochoa, and Kristin McDougall. "Chronology and Paleoenvironment of the Tunga Formation, a new lowermost Miocene sequence in the East Pisco Basin of southern Peru." Stratigraphy 21, no. 3 (2024): 189–224. http://dx.doi.org/10.29041/strat.21.3.02.

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The East Pisco Basin, occupying the coastal plain of Peru between 13°S and 16°S, is widely known for its extensive Eocene to Quaternary biosiliceous deposits and excellent preservation of fossil marine vertebrates. Biochronologic studies published over the past 35 years record a hiatus of about 13 million years (*32–19 Ma) separating the youngest Paleogene deposits (Otuma Formation) from the oldest Neogene deposits (Chilcatay Formation). We describe a newly identified Lower Miocene depositional sequence that lies below documented Chilcatay strata, rich in diatoms and benthic foraminifers, whic
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Pachac-Huerta, Yenica, Waldo Lavado-Casimiro, Melania Zapana, and Robinson Peña. "Understanding Spatio-Temporal Hydrological Dynamics Using SWAT: A Case Study in the Pativilca Basin." Hydrology 11, no. 10 (2024): 165. http://dx.doi.org/10.3390/hydrology11100165.

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This study investigates the hydrological dynamics of the Pativilca Basin in the Southern Hemisphere using the SWAT (Soil and Water Assessment Tool) model. Seventy-seven watersheds across a mountainous region were analyzed using elevation data, land cover, soil type, and gridded meteorological products (RAIN4PE and PISCO) for hydrological simulations. Watershed delineation, aided by a Digital Elevation Model, enabled the identification of critical drainage points and the definition of Hydrological Response Units (HRUs). The model calibration and validation, performed using the SWAT-CUP with the
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Farias de Reyes, Marina, Eduardo Chávarri-Velarde, Valeria Cotrina, Pierina Aguilar, and Laura Vegas. "Space-Time Variability of Maximum Daily Rainfall in Piura River Basin in Peru Related to El Niño Occurrence." Water 16, no. 23 (2024): 3452. https://doi.org/10.3390/w16233452.

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This study analyzes hydrometeorological data (1950–2023) to examine the signatures of El Niño and La Niña events and assess their impact on rainfall distribution in the Piura Region, Peru. Using data from 23 stations, high-resolution gridded rainfall datasets (PISCO), and oceanic–atmospheric indices we investigated the frequency, intensity, and spatial variability of these events in the Piura River Basin (PRB). Return periods for very strong El Niño and La Niña events are 25 and 19 years, respectively, compared to 2 years for neutral conditions. Over the past 30 years, the recurrence of Coasta
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30

Coletti, Giovanni, Giulia Bosio, Alberto Collareta, et al. "Biostratigraphic, evolutionary, and paleoenvironmental significance of the southernmost lepidocyclinids of the Pacific coast of South America (East Pisco Basin, southern Peru)." Journal of South American Earth Sciences 96 (December 2019): 102372. http://dx.doi.org/10.1016/j.jsames.2019.102372.

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31

Gariboldi, Karen, Anna Gioncada, Giulia Bosio, et al. "The dolomite nodules enclosing fossil marine vertebrates in the East Pisco Basin, Peru: Field and petrographic insights into the Lagerstätte formation." Palaeogeography, Palaeoclimatology, Palaeoecology 438 (November 2015): 81–95. http://dx.doi.org/10.1016/j.palaeo.2015.07.047.

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32

Rustichelli, Andrea, Claudio Di Celma, Emanuele Tondi, Patrick Baud, and Sergio Vinciguerra. "Fibrous gypsum veins as diffuse features and within fault zones: the case study of the Pisco Basin (Ica desert, southern Peru)." Journal of the Geological Society 173, no. 3 (2016): 405–18. http://dx.doi.org/10.1144/jgs2015-084.

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33

Malinverno, Elisa, Giulia Bosio, Claudio Di Celma, et al. "(Bio)stratigraphic overview and paleoclimatic-paleoceanographic implications of the middle-upper Eocene deposits from the Ica River Valley (East Pisco Basin, Peru)." Palaeogeography, Palaeoclimatology, Palaeoecology 578 (September 2021): 110567. http://dx.doi.org/10.1016/j.palaeo.2021.110567.

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34

del Aguila, Sandra, and Francisco Espinoza-Montes. "Impacto del cambio climático en las descargas futuras de una cuenca altoandina de Perú al 2100." Tecnología y ciencias del agua 15, no. 1 (2024): 111–55. http://dx.doi.org/10.24850/j-tyca-15-01-03.

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El objetivo de esta investigación fue analizar el impacto del cambio climático en el comportamiento de las descargas mensuales en la cuenca Anya, afluente del Mantaro, Junín, al 2100, con el modelo SWAT (Soil and Water Assessment Tool). Se obtuvieron datos grillados diarios de precipitación y temperaturas de PISCO (Peruvian Interpolated data of the SENAMHI’s Climatological and Hydrological Observations) entre 1981 y 2015, y caudales promedio mensuales medidos en la estación hidrométrica Anya. Para el análisis del efecto espacio temporal del cambio climático en la temperatura y precipitación, y
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Cadena, Edwin, Juan Abella, and Maria Gregori. "The first Oligocene sea turtle (Pan-Cheloniidae) record of South America." PeerJ 6 (March 23, 2018): e4554. http://dx.doi.org/10.7717/peerj.4554.

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The evolution and occurrence of fossil sea turtles at the Pacific margin of South America is poorly known and restricted to Neogene (Miocene/Pliocene) findings from the Pisco Formation, Peru. Here we report and describe the first record of Oligocene (late Oligocene, ∼24 Ma) Pan-Cheloniidae sea turtle remains of South America. The fossil material corresponds to a single, isolated and well-preserved costal bone found at the Montañita/Olón locality, Santa Elena Province, Ecuador. Comparisons with other Oligocene and extant representatives allow us to confirm that belongs to a sea turtle character
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Collareta, Alberto, René Kindlimann, Alessio Baglioni, et al. "Dental Morphology, Palaeoecology and Palaeobiogeographic Significance of a New Species of Requiem Shark (Genus Carcharhinus) from the Lower Miocene of Peru (East Pisco Basin, Chilcatay Formation)." Journal of Marine Science and Engineering 10, no. 10 (2022): 1466. http://dx.doi.org/10.3390/jmse10101466.

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Nowadays, the requiem sharks comprise one of the most diverse and widespread families of selachians, i.e., Carcharhinidae. Among the carcharhinids, the genus Carcharhinus has the largest number of living species, namely, at least 35. Known from fossils as old as the Cretaceous, the requiem sharks did not significantly radiate before the Eocene (when Carcharhinus also appeared), and their diversification mainly occurred in Neogene times. Here, we describe a new species of requiem shark, Carcharhinus dicelmai sp. nov., based on fossil teeth from Lower Miocene (18.4–18.1 Ma) strata of the Chilcat
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37

Villafuerte, Elmer Moreno, and Eleazar Chuchon Angulo. "Evaluating Statistical Bias Correction Techniques to Enhance Precipitation Projections in the Cachi Basin, Peruvian Andes." Revista de Gestão Social e Ambiental 18, no. 11 (2024): e09204. http://dx.doi.org/10.24857/rgsa.v18n11-005.

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Introduction: To assess the impact of climate change on watersheds, accurate meteorological data are required. Regional Climate Model (RCM) data sets are widely used to feed ecological and hydrological models. However, in Andean regions such as the Peruvian Andes such as the Cachi basin, the scarcity of observation stations generates biases in the RCMs. This study evaluates the performance effect of a simple (Linear Scaling) and complex (Power Transformation and Distribution Mapping) statistical bias correction technique applied on the set of 10 RCM simulations with and without bias correction
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DeVries, Thomas J., John A. Barron, Mario Urbina-Schmitt, Diana Ochoa, Raúl Esperante, and Lawrence W. Snee. "The Miocene stratigraphy of the Laberinto area (Río Ica Valley) and its bearing on the geological history of the East Pisco Basin (south-central Peru)." Journal of South American Earth Sciences 111 (November 2021): 103458. http://dx.doi.org/10.1016/j.jsames.2021.103458.

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39

Coletti, Giovanni, Alberto Collareta, Giulia Bosio, Mario Urbina-Schmitt, and John Buckeridge. "Perumegabalanus calziai gen. et sp. nov., a new intertidal megabalanine barnacle from the early Miocene of Peru." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 294, no. 2 (2019): 197–212. http://dx.doi.org/10.1127/njgpa/2019/0856.

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Living members of the tribe Austromegabalanini are large balanid barnacles (Crustacea: Cirripedia: Neobalanoformes) that live in temperate and cold waters of the Southern Hemisphere. During the Neogene, however, the austromegabalanines also inhabited the Northern Hemisphere, as well as some low- latitude tropical environments. This paper describes a new taxon of austromegab-alanines, Perumegabalanus calziai gen. et sp. nov., from the shallow-marine, nearshore, lower Miocene (19 to 17 Ma, Burdigalian) deposits of the Chilcatay Formation (East Pisco Basin, southern Peru). Among austromegabalanin
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Bianucci, Giovanni, Claudio Di Celma, Alberto Collareta, et al. "Fossil marine vertebrates of Cerro Los Quesos: Distribution of cetaceans, seals, crocodiles, seabirds, sharks, and bony fish in a late Miocene locality of the Pisco Basin, Peru." Journal of Maps 12, no. 5 (2016): 1037–46. http://dx.doi.org/10.1080/17445647.2015.1115785.

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41

Moya-Álvarez, Aldo S., Daniel Martínez-Castro, José L. Flores, and Yamina Silva. "Sensitivity Study on the Influence of Parameterization Schemes in WRF_ARW Model on Short- and Medium-Range Precipitation Forecasts in the Central Andes of Peru." Advances in Meteorology 2018 (2018): 1–16. http://dx.doi.org/10.1155/2018/1381092.

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A sensitivity study of the performance of the Weather Research and Forecasting regional model (WRF, version 3.7) to the use of different microphysics, cumulus, and boundary layer parameterizations for short- and medium-term precipitation forecast is conducted in the Central Andes of Peru. Lin-Purdué, Thompson, and Morrison microphysics schemes were tested, as well as the Grell–Freitas, Grell 3d, and Betts–Miller–Janjic cumulus parameterizations. The tested boundary layer schemes were the Yonsei University and Mellor–Yamada–Janjic. A control configuration was defined, using the Thompson, Grell–
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42

Filippelli, G. M., M. L. Delaney, R. E. Garrison, S. K. Omarzai, and R. J. Behl. "Phosphorus accumulation rates in a Miocene low oxygen basin: The Monterey Formation (Pismo Basin), California." Marine Geology 116, no. 3-4 (1994): 419–30. http://dx.doi.org/10.1016/0025-3227(94)90055-8.

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Liddicoat, Joseph C. "Palaeomagnetism of the Pico Formation, Santa Paula Creek, Ventura Basin, California." Geophysical Journal International 110, no. 2 (1992): 267–75. http://dx.doi.org/10.1111/j.1365-246x.1992.tb00872.x.

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Nieves-Vilchez, Ines Aberlí, Hiram Joshua Castillo-Infante, Josué Isac Carillo-Espinoza, and Noé Benjamín Pampa-Quispe. "Estudio hidrológico de una cuenca para la evaluación del potencial de una pico central hidroeléctrica en una zona rural." Tecnología y ciencias del agua 13, no. 1 (2022): 292–332. http://dx.doi.org/10.24850/j-tyca-2022-01-07.

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Rudolph, Kurt W., Wolfgang Schlager, and Kevin T. Biddle. "Seismic models of a carbonate foreslope-to-basin transition, Picco di Vallandro, Dolomite Alps, northern Italy." Geology 17, no. 5 (1989): 453. http://dx.doi.org/10.1130/0091-7613(1989)017<0453:smoacf>2.3.co;2.

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46

Schouten, Stefan, Martin Schoell, W. Irene C. Rijpstra, Jaap S. Sinninghe Damsté, and Jan W. de Leeuw. "A molecular stable carbon isotope study of organic matter in immature Miocene Monterey sediments, Pismo basin." Geochimica et Cosmochimica Acta 61, no. 10 (1997): 2065–82. http://dx.doi.org/10.1016/s0016-7037(97)00062-8.

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Langhals, Heinz, and Sigrid Saulich. "Chromophores as Elements of Structure for Pico Technology Optical Computers." Zeitschrift für Naturforschung B 58, no. 7 (2003): 695–97. http://dx.doi.org/10.1515/znb-2003-0715.

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The transfer of the energy of optical excitation between the different chromophores of anthraquinone and perylene dyes has been controlled by their relative orientation. Such assemblies are basic components for optical computers on the picometer scale.
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Zakariz, Naufal Praska, and Anggara Trisna Nugraha. "The Effect of Inlet Notch Variations on Turbine Speed in Pico-hydro Power Plants." Journal of Electronics, Electromedical Engineering, and Medical Informatics 4, no. 1 (2022): 35–41. http://dx.doi.org/10.35882/jeeemi.v4i1.4.

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Energy is an important element in the continuity of human activities. Indonesia has the potential to produce 94.3GigaWatt of electricity in the hydropower sector, but only a few can be utilized, which is only 4.2GigaWatt [1]. This study aims to utilize renewable energy that has not been utilized optimally, especially in Indonesia. This study exploits the potential of water flow from the Coban Wonoasri River, Bangun Village, Munjungan District, Trenggalek Regency which has a low head but has a fairly heavy discharge. The basin cone for making vortex flow has a canal length of 1450mm, a canal wi
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Carrick, Hunter J., Emon Butts, Daniella Daniels, et al. "Variation in the abundance of pico, nano, and microplankton in Lake Michigan: Historic and basin-wide comparisons." Journal of Great Lakes Research 41 (2015): 66–74. http://dx.doi.org/10.1016/j.jglr.2015.09.009.

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Trinidad Hernández, Oswaldo, Katrin Sieron, and Francisco Córdoba Montiel. "Susceptibilidad a erosión hídrica y procesos gravitacionales en la subcuenca de alta montaña del río Jamapa, Veracruz, México." UVserva, no. 8 (October 25, 2019): 16–28. http://dx.doi.org/10.25009/uvs.v0i8.2632.

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En el presente trabajo se determinó la susceptibilidad actual a procesos de erosión hídrica y procesos gravitacionales en la subcuenca de alta montaña del río Jamapa en el flanco Norte del volcán Citlaltépetl o Pico de Orizaba. El estudio se llevó a cabo mediante el empleo de Sistemas de Información Geográfica (SIG), con la aplicación los modelos USLE y Mora-Vahrson. Los resultados mostraron una concordancia de ambos modelos de acuerdo con la distribución de los mayores grados de susceptibilidad. Contrario a lo que se esperaba, los modelos arrojaron mayores susceptibilidades tanto de erosión h
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