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84 results for “Meridion”
FIGURES 1–10. Larinia dubia n in Two new species of orb-weaving spiders of the genus Larinia (Araneae, Araneidae) in meridional Brazil
FIGURES 1–10. Larinia dubia n. sp. 1, 3, Male (holotype, MCN 52123). 2, 4, Female (paratype, MCN 52122). 5–7, Male palp. 8–10, Epigynum. 1, 2, Dorsal. 3, 4, Ventral. 5, Prolateral. 6, Retrolateral. 7, Ventral. 8, Ventral. 9, Posterior. 10, Posterior, clarified. A, terminal apophysis; C, conductor; E, embolus; M, median apophysis; S, scape; T, tegulum. Scale bars: 3 mm (1–4); 0.25 mm (5–10). FIGURES 11–19. Larinia robusta n. sp. (male holotype and female paratype, MCN 25410). 11, 13, Male. 12, 14, Female. 18–19, Epigynum. 11, 12, Dorsal. 13, 14, Ventral. 15–17, Male palp. 15, Prolateral. 16, Retrolateral. 17, Ventral. 18, Ventral. 19, Posterior. Scale bars: 3 mm (11–14); 0.25 mm (15–19).
FIGURES 20–25. 20, 21 in Two new species of orb-weaving spiders of the genus Larinia (Araneae, Araneidae) in meridional Brazil
FIGURES 20–25. 20, 21, Larinia tucuman Harrod, Levi & Leibensperger, 1991 (MCN 25201). 22, 23, Larinia dubia n. sp. (MCN 39126). 24, 25, Larinia robusta n. sp. (MCN 25410). 20, 22, 24, Male palp, prolateral. 21, 23, 25, Median apophysis, detail. Scale bars: 0.2 mm (20, 22, 24); 0.1 mm (21, 23, 25).
Data supporting Satellite in-situ electron density observations of the mid-latitude storm enhanced density on the noon meridional plane in the F region during the 20 November 2003 magnetic storm
<p>This is the data for the submitted paper: Satellite in-situ electron density observations of the mid-latitude storm enhanced density on the noon meridional plane in the F region during the 20 November 2003 magnetic storm. The data contains five files. The file NE_TGWeimer_2003324 is the electron density (NE) data along the CHAMP orbit on Nov 20, 2003. The file TGSED4_Mlat30_2003324 is the NE, HMF2, WI_ExB, VI_ExB and VN at Mlat = 30 on the noon meridional plane (MLT = 12 hr) in the Northern hemisphere on Nov 20, 2003. The temporal resolution is 1-min. The file TGSED4_Mlat60_2003324 is the NE, HMF2, WI_ExB, VI_ExB and VN at Mlat = 60 on the noon meridional plane (MLT = 12 hr) in the Northern hemisphere on Nov 20, 2003. The temporal resolution is 1-min. The file TGSED3_Mlat30_2003324 is the NE at Mlat = 30 as a function of MLT and UT. The temporal resolution is 5-min. The file TGSED3_Mlat60_2003324 is the NE at Mlat = 60 as a function of MLT and UT. The temporal resolution is 5-min.</p>
Ocean Meridional Heat Transport Values
<p>This dataset includes data for Figures 2, 4, 6, 10 and 12 of the "Observation-based Estimate of Global and Basin Ocean Meridional Heat Transport Time Series" paper. This paper is published through the Journal of Climate (2019) and by authors, Kevin E. Trenberth, Yongxin Zhang, John T. Fasullo and Lijing Cheng. The data files associated with this dataset provides tabular values and are for general use.</p>
On following pages: 174. Small Big-eared Brown Bat (Histiotus montanus);, 175. Thomas's Big-eared Brown Bat (Histiotus laephotis); 176. Common Big-eared Brown Bat (Histiotus macrotus); 177. Southern Big-eared Brown Bat (Histiotus magellanicus); 178. Big Brown Bat (Eptesicus fuscus); 179. Guadeloupe Serotine (Eptesicus guadeloupensis); 180. Diminutive Serotine (Eptesicus diminutus); 181. Little Black Serotine (Eptesicus andinus); 182. Chiriguinan Serotine (Eptesicus chiriquinus); 183. Argentine Serotine (Eptesicus furinalis); 184. Harmless Serotine (Eptesicus innoxius); 185. Brazilian Serotine (Eptesicus brasiliensis); 186. Taddei's Serotine (Eptesicus taddeii); 187. Ulapes Serotine (Eptesicus ulapesensis); 188. Horn-skinned Serotine (Eptesicus floweri); 189. Lagos Serotine (Eptesicus platyops); 190. Long-tailed Serotine (Eptesicus hottentotus); 191. Ognev's Serotine (Eptesicus ognevi); 192. Anatolian Serotine (Eptesicus anatolicus); 193. Botta's Serotine (Eptesicus bottae); 194. Meridional Serotine (Eptesicus isabellinus); 195. Oriental Serotine (Eptesicus pachyomus); 196. Eurasian Serotine (Eptesicus serotinus); 197. Northern Serotine (Eptesicus nilssonil); 198. Sombre Serotine (Eptesicus tate); 199. Gobi Serotine (Eptesicus gobiensis), 200. Japanese Serotine (Eptesicus japonensis);, 201. Thick-eared Serotine (Eptesicus pachyotis). in Vespertilionidae
On following pages: 174. Small Big-eared Brown Bat (Histiotus montanus);, 175. Thomas's Big-eared Brown Bat (Histiotus laephotis); 176. Common Big-eared Brown Bat (Histiotus macrotus); 177. Southern Big-eared Brown Bat (Histiotus magellanicus); 178. Big Brown Bat (Eptesicus fuscus); 179. Guadeloupe Serotine (Eptesicus guadeloupensis); 180. Diminutive Serotine (Eptesicus diminutus); 181. Little Black Serotine (Eptesicus andinus); 182. Chiriguinan Serotine (Eptesicus chiriquinus); 183. Argentine Serotine (Eptesicus furinalis); 184. Harmless Serotine (Eptesicus innoxius); 185. Brazilian Serotine (Eptesicus brasiliensis); 186. Taddei's Serotine (Eptesicus taddeii); 187. Ulapes Serotine (Eptesicus ulapesensis); 188. Horn-skinned Serotine (Eptesicus floweri); 189. Lagos Serotine (Eptesicus platyops); 190. Long-tailed Serotine (Eptesicus hottentotus); 191. Ognev's Serotine (Eptesicus ognevi); 192. Anatolian Serotine (Eptesicus anatolicus); 193. Botta's Serotine (Eptesicus bottae); 194. Meridional Serotine (Eptesicus isabellinus); 195. Oriental Serotine (Eptesicus pachyomus); 196. Eurasian Serotine (Eptesicus serotinus); 197. Northern Serotine (Eptesicus nilssonil); 198. Sombre Serotine (Eptesicus tate); 199. Gobi Serotine (Eptesicus gobiensis), 200. Japanese Serotine (Eptesicus japonensis);, 201. Thick-eared Serotine (Eptesicus pachyotis).
Severe drought conditions in northern East Asia during the early Pliocene caused by weakened Pacific meridional temperature gradient
<p>The evolution of hydroclimate in East Asia during the Pliocene – a potential analogue of the future greenhouse climate – remains highly uncertain. Here we reconstruct changes in the hydroclimate of Northern China during this epoch. Our results reveal previously undocumented severe drought conditions that persisted through the early Pliocene with a significantly greater magnitude than suggested by other records. Using a broad hierarchy of climate simulations, we find that reduction in the Pacific meridional sea surface temperature gradient has particularly strong impacts on precipitation over Northern China, which suggests its key role in maintaining drought conditions during the early Pliocene. The weaker Pacific meridional SST gradient causes the weakening of the East Asian summer monsoon precipitation over this region via a reduction of atmospheric northward moisture transport from the ocean, which enhances aridity inland. Our results highlight the fundamental control of the tropical ocean on the extra-tropical hydrological cycle.</p>
Data for "Impacts of an active Pacific Meridional Overturning Circulation on the Pliocene climate and hydrological cycle"
<p>Post-Processing Scripts and Data for the Paper<br>Title: Impacts of an Active Pacific Meridional Overturning Circulation on the Pliocene Climate and Hydrological Cycle<br>Authors: Minmin Fu, Alexey Fedorov<br>Publication Year: 2024<br>Contact: minmin.fu@yale.edu</p> <p>Overview<br>This repository contains the post-processing scripts and data used in the paper. It includes Jupyter notebooks for data analysis and plot generation, as well as the GCM output and utilities for adding land-sea masks and proxy sites.</p> <p>Repository Structure<br>notebooks/: Jupyter notebooks for analyzing data and creating plots.<br>data/: GCM output files for reproducing all figures in the paper.<br>utilities/: Functions for adding the land-sea mask and proxy sites.<br>PlioMIP2/: PlioMIP2 boundary conditions.</p> <p>Data<br>The data directory contains the GCM output files necessary for reproducing all figures. Ensure you have the necessary storage space as these files may be large.</p> <p>Utilities<br>The utilities directory contains utility functions, including:</p> <p>Land-Sea Mask Functions: Scripts to apply land-sea masks to the data.<br>Proxy Site Functions: Scripts to integrate proxy site data into the analysis.<br>The PlioMIP2 directory contains the boundary condition files used for the PlioMIP2 experiments.</p>
Supplementary Material from: Meridional shifts of the Southern Hemisphere westerlies during the early Cenozoic
<p><span>Dataset of median grain size, siliciclastic mass accumulation rate (MAR<sub>siliciclastic</sub>), clay minerals, and major and trace elements of siliciclastic fractions at <span>International Ocean Discovery Program (IODP) </span>Site U1514 generated from the study: Meridional shifts of the Southern Hemisphere westerlies during the early Cenozoic.</span></p>
Roles of the Labrador Current in the Atlantic Meridional Overturning Circulation responses to greenhouse warming
<p>This archive contains data and MATLAB code used to generate figures in the paper "Roles of the Labrador Current in the Atlantic Meridional Overturning Circulation responses to greenhouse warming". </p>
An observation-based estimate of the Atlantic meridional freshwater transport
Open the record for dataset details and reuse information.
Nonkinematic solar dynamo models with double-cell meridional circulation
<p>MESA inlists for <a href="https://ui.adsabs.harvard.edu/#abs/2018JASTP.179..185P/abstract">Nonkinematic solar dynamo models with double-cell meridional circulation</a></p>
A Dataset for Response of Oceanic Meridional Overturning Circulation to Vegetation Removal on Different Continents
Open the record for dataset details and reuse information.
Nonstationarity of the Atlantic Meridional Overturning Circulation's fingerprint on sea surface temperature
<p>Associated data for "Nonstationarity of the Atlantic Meridional Overturning Circulation’s fingerprint on sea surface temperature". V2 updated to include datasets for the supplemental information.</p>
Data and code for : Madden Julian Oscillation moves faster as the meridional moisture gradient intensifies in a warming world
<p>Data and code related to the research article titled “Madden Julian Oscillation moves faster as the meridional moisture gradient intensifies in a warming world,” published in Geophysical Research Letters.</p>
Local Time Variations of Quiet Time Meridional Winds during June and December based on ICON Observations and Numerical Simulations
<p>The file named '<a href="../api/records/12139509/draft/files/geomagnetic%20index.mat/content" target="_blank" rel="noopener noreferrer">geomagnetic index</a>' includes Kp, F10.7p, By and Bz indices, AE and Dst indices. The file named '<a href="../api/records/12139509/draft/files/MWjym12.mat/content" target="_blank" rel="noopener noreferrer">MWjym06</a>', '<a href="../api/records/12139509/draft/files/MWjym12.mat/content" target="_blank" rel="noopener noreferrer">MWjym12</a>' are the meridional winds of ICON observations in June and December. The file named '<a href="../api/records/12139509/draft/files/VN_mean06.mat/content" target="_blank" rel="noopener noreferrer">VN_mean06</a>', '<a href="../api/records/12139509/draft/files/VN_mean06.mat/content" target="_blank" rel="noopener noreferrer">VN_mean12</a>' , '<a href="../api/records/12139509/draft/files/VN_mean06.mat/content" target="_blank" rel="noopener noreferrer">VNnotide_mean06</a>','<a href="../api/records/12139509/draft/files/VN_mean06.mat/content" target="_blank" rel="noopener noreferrer">VNnotide_mean12</a>' include the parameters of TIEGCM simulated meridional winds and the forcing terms with and without tides in June and December. The file named 'F107_70' is the simulation in December in F10.7=70.</p>
Figure Data for Oka et al. (2021) "Glacial mode shift of the Atlantic meridional overturning circulation by warming over the Southern Ocean"
<p>Figure Data for Oka et al. (2021) "Glacial mode shift of the Atlantic meridional overturning circulation by warming over the Southern Ocean" </p>
Data for the figures of Ando et al. entitled "Hysteresis of the glacial Atlantic Meridional Overturning Circulation controlled by thermal feedbacks."
<p>Data for the figures of Ando et al. entitled "Hysteresis of the glacial Atlantic Meridional Overturning Circulation controlled by thermal feedbacks."</p>
The Role of Atlantic Basin Geometry in Meridional Overturning Circulation
<p>Climatology data for manuscript: "The Role of Atlantic Basin Geometry in Meridional Overturning Circulation"</p> <p>We present idealized simulations to explore how the shape of eastern and western continental boundaries along the Atlantic influence the Atlantic Meridional Overturning Circulation (AMOC). We use a state-of-the art ocean—sea-ice model (MOM6 and SIS2) with idealized, zonally-symmetric surface forcing and a range of idealized continental configurations with a large, Pacific-like basin and a small, Atlantic-like basin. We perform simulations with five coastline geometries along the Atlantic-like basin that range from coastlines that are straight to coastlines shaped like the coasts of the American and African continents.</p>
Meridional wave power distribution data for article "Latitudinal Dependence of Ground VLF Transmitter Wave Power in the Inner Magnetosphere"
<p>The data are the meridional wave power distribution for the four VLF transmitters: NWC, NAA, NML, and NLK in the inner magnetosphere. Each transmitter has a .mat file, and in each data file, we provide the meridional wave power distribution for both ray tracing simulation (parameter "rt") and ERG observation (parameter "erg"). In each distribution data, the variables "x2d" and "z2d" are the cartesian coordinates in the meridional plane in the unit of Re (the Eearth's radius). x2d=r*cos(theta) and z2d=r*sin*(theta), where r is the radius from the Earth's center, and theta is the magnetic latitude. The variable "power" is the corresponding transmitter wave power in the unit of V^2/m^2.</p>
FIGURES 1–3 in Two new species of the diatom genus Meridion (Bacillariophyta, Tabellariaceae) from Aleutian Islands
FIGURES 1–3. Maps showing Unalaska Island location in chain of Aleutian Islands and material collection site.
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