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Author |
O'Brien, J.; Richards, T. S.; Davis, A. C. |
Title |
The effect of El Nino on U.S. landfalling hurricanes |
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$loc['typeMagazine Article'] |
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1996 |
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Bulletin of the American Meteorological Society |
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77 |
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4 |
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773-774 |
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COAPS @ mfield @ |
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715 |
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Vinayachandran, P. N.; Davidson, Fraser; Chassignet, E. P. |
Title |
Towards joint assessments, modern capabilities and new links for ocean prediction systems |
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$loc['typeJournal Article'] |
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2020 |
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Bulletin of the American Meteorological Society |
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Bull. Amer. Meteor. Soc. |
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101 |
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4 |
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Approximately 260 individuals from forecasting centers, research laboratories, academia, and industry representing 40 countries met to discuss recent developments in operational oceanography and brainstorm about the future directions of ocean prediction services. |
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COAPS @ user @ |
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1091 |
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Author |
Zou, S.; Lozier, M.S.; Xu, X. |
Title |
Latitudinal Structure of the Meridional Overturning Circulation Variability on Interannual to Decadal Time Scales in the North Atlantic Ocean |
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$loc['typeJournal Article'] |
Year |
2020 |
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Journal of Climate |
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J. Climate |
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33 |
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9 |
Pages |
3845-3862 |
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Deep convection; Ocean circulation; Thermocline circulation |
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The latitudinal structure of the Atlantic meridional overturning circulation (AMOC) variability in the North Atlantic is investigated using numerical results from three ocean circulation simulations over the past four to five decades. We show that AMOC variability south of the Labrador Sea (53°N) to 25°N can be decomposed into a latitudinally coherent component and a gyre-opposing component. The latitudinally coherent component contains both decadal and interannual variabilities. The coherent decadal AMOC variability originates in the subpolar region and is reflected by the zonal density gradient in that basin. It is further shown to be linked to persistent North Atlantic Oscillation (NAO) conditions in all three models. The interannual AMOC variability contained in the latitudinally coherent component is shown to be driven by westerlies in the transition region between the subpolar and the subtropical gyre (40°–50°N), through significant responses in Ekman transport. Finally, the gyre-opposing component principally varies on interannual time scales and responds to local wind variability related to the annual NAO. The contribution of these components to the total AMOC variability is latitude-dependent: 1) in the subpolar region, all models show that the latitudinally coherent component dominates AMOC variability on interannual to decadal time scales, with little contribution from the gyre-opposing component, and 2) in the subtropical region, the gyre-opposing component explains a majority of the interannual AMOC variability in two models, while in the other model, the contributions from the coherent and the gyre-opposing components are comparable. These results provide a quantitative decomposition of AMOC variability across latitudes and shed light on the linkage between different AMOC variability components and atmospheric forcing mechanisms. |
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0894-8755 |
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COAPS @ user @ |
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1106 |
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Author |
Mende, M.; Misra, V. |
Title |
Time to Flatten the Curves on COVID-19 and Climate Change. Marketing Can Help |
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$loc['typeJournal Article'] |
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2020 |
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Journal of Public Policy & Marketing |
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Journal of Public Policy & Marketing |
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The health, economic, and social impact of the COVID-19 pandemic is unprecedented in our lifetime, and no individual in this globalized, interconnected world is immune from its effects. This pandemic is a fundamental challenge for consumers, companies, and governments. Against this background, our commentary underscores linkages between public health, environment, and economy and explores how lessons from COVID-19 can help prevent other large-scale disasters.1 We focus on global climate change (GCC), because rising temperatures increase the likelihood of future pandemics.2 Accordingly, experts consider GCC “the largest public health threat of the century” (Wyns 2020). Although societal crises are underresearched in marketing, we propose that marketers should add their expertise to help avoid future crises. Notably, the Journal of Public Policy & Marketing (JPP&M) is uniquely positioned as a premier outlet for corresponding research at the intersection of marketing and policy. |
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COAPS @ user @ |
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1117 |
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Author |
Laurencin, C.; Misra, V. |
Title |
Characterizing the Variations of the motion of the North Atlantic tropical cyclones |
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$loc['typeJournal Article'] |
Year |
2018 |
Publication |
Meteorology and Atmospheric Physics |
Abbreviated Journal |
Meteorol Atmos Phys |
Volume |
130 |
Issue |
303 |
Pages |
1-12 |
Keywords |
climatology; interannual scales; environment |
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In this study, we examine the seasonal and interannual variability of the North Atlantic (NATL) tropical cyclone (TC) motion from the historical Hurricane Database (HURDAT2) over the period 1988-2014. We characterize these motions based on their position, lifecycle, and seasonal cycle. The main findings of this study include: (1) of the 11,469 NATL TC fixes examined between 1988 and 2014, 81% of them had a translation speed of < 20 mph; (2) TCs in the deep tropics of the NATL are invariably slow-moving in comparison with TCs in higher latitudes. Although fast-moving TCs (> 40 mph) are exclusively found north of 30 N, the slow-moving TCs have a wide range of latitude. This is largely a consequence of the background steering flow being weaker (stronger) in the tropical (higher) latitudes with a minimum around the subtropical latitudes of NATL; (3) there is an overall decrease in the frequency of all categories of translation speed of TCs in warm relative to cold El Niño Southern Oscillation (ENSO) years. However, in terms of the percentage change, TCs with a translation speed in the range of 10-20 mph display the most change (42%) in warm relative to cold ENSO years; and (4) there is an overall decrease in frequency across all categories of TC translation speed in small relative to large Atlantic Warm Pool years, but in terms of percentage change in the frequency of TCs, there is a significant and comparable change in the frequency over a wider range of translation speeds than the ENSO composites. This last finding suggests that Atlantic Warm Pool variations have a more profound impact on the translation speed of Atlantic TCs than ENSO. |
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COAPS @ rl18 @ |
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991 |
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Author |
Glazer, R. H.; Misra, V. |
Title |
Ice versus liquid water saturation in simulations of the Indian summer monsoon |
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$loc['typeJournal Article'] |
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2018 |
Publication |
Climate Dynamics |
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Indian monsoon; Regional modeling; Saturation vapor pressure; Cloud microphysics scheme |
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COAPS @ mfield @ |
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943 |
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Author |
Bellow, J., A. Mokssit, J. O'Brien, and R. Sebbari |
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Building national and specialised climate services |
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$loc['typeBook Chapter'] |
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2008 |
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Seasonal Climate: Forecasting and Managing Risk |
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315-349 |
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Springer |
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Troccoli, A.; Harrison, M.; Anderson, D. L. T.; Mason, S. |
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$loc['no'] |
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COAPS @ mfield @ |
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682 |
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Bellow, J. G.; Nair, P. K. R.; Martin, T. A. |
Title |
Tree-Crop Interactions in Fruit Tree-based Agroforestry Systems in the Western Highlands of Guatemala: Component Yields and System Performance |
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$loc['typeBook Chapter'] |
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2008 |
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Toward Agroforestry Design. Advances in Agroforestry |
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4 |
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Springer |
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Dordrecht |
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Jose, S.; Gordon, A. M. |
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COAPS @ mfield @ |
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906 |
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Deng, J.; Wu, Z.; Zhang, M.; Huang, N.E.; Wang, S.; Qiao, F. |
Title |
Using Holo-Hilbert spectral analysis to quantify the modulation of Dansgaard-Oeschger events by obliquity |
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$loc['typeJournal Article'] |
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2018 |
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Quaternary Science Reviews |
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Quaternary Science Reviews |
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192 |
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282-299 |
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Pleistocene; Paleoclimatology; Greenland; Antarctica; Data treatment; Data analysis; Dansgaard-oeschger (DO) events; Obliquity forcing; Phase preference; Holo-hilbert spectral analysis; Amplitude modulation; EMPIRICAL MODE DECOMPOSITION; GREENLAND ICE-CORE; NONSTATIONARY TIME-SERIES; ABRUPT CLIMATE-CHANGE; LAST GLACIAL PERIOD; NORTH-ATLANTIC; MILLENNIAL-SCALE; RECORDS; VARIABILITY; CYCLE |
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Astronomical forcing (obliquity and precession) has been thought to modulate Dansgaard-Oeschger (DO) events, yet the detailed quantification of such modulations has not been examined. In this study, we apply the novel Holo-Hilbert Spectral Analysis (HHSA) to five polar ice core records, quantifying astronomical forcing's time-varying amplitude modulation of DO events and identifying the preferred obliquity phases for large amplitude modulations. The unique advantages of HHSA over the widely used windowed Fourier spectral analysis for quantifying astronomical forcing's nonlinear modulations of DO events is first demonstrated with a synthetic data that closely resembles DO events recorded in Greenland ice cores (NGRIP, GRIP, and GISP2 cores on GICC05 modelext timescale). The analysis of paleoclimatic proxies show that statistically significantly more frequent DO events, with larger amplitude modulation in the Greenland region, tend to occur in the decreasing phase of obliquity, especially from its mean value to its minimum value. In the eastern Antarctic, although statistically significantly more DO events tend to occur in the decreasing obliquity phase in general, the preferred phase of obliquity for large amplitude modulation on DO events is a segment of the increasing phase near the maximum obliquity, implying that the physical mechanisms of DO events may be different for the two polar regions. Additionally, by using cross-spectrum and magnitude-squared analyses, Greenland DO mode at a timescale of about 1400 years leads the Antarctic DO mode at the same timescale by about 1000 years. (C) 2018 Elsevier Ltd. All rights reserved. |
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0277-3791 |
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COAPS @ user @ |
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971 |
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Stukel, M.R.; Kelly, T.B. |
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The carbon: 234Thorium ratios of sinking particles in the California current ecosystem 2: Examination of a thorium sorption, desorption, and particle transport model |
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Marine Chemistry |
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Marine Chemistry |
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0304-4203 |
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COAPS @ user @ |
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1037 |
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