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1. Thank You to Our 2020 Peer Reviewers

Author

Rajaram, Harihar, Camargo, Suzana, Cappa, Christopher, Carey, Rebecca, Cory, Rose, Dombard, Andrew, Donohue, Kathleen, Flesch, Lucy, Giannini, Alessandra, Gu, Yu, Hayes, Gavin, Hogg, Andrew, Huber, Christian, Ivanov, Valeriy, Jacobsen, Steven, Korte, Monika, Lu, Gang, Morlighem, Mathieu, Magnusdottir, Gudrun, Opher, Merav, Patricola, Christina, Prieto, Germán, Qiu, Bo, Ritsema, Jeroen, Sprintall, Janet, Su, Hui, Sun, Daoyuan, Thornton, Joel, Trouet, Valerie, Wang, Kaicun, Whalen, Caitlin, White, Angelicque, and Yau, Andrew

Subjects
Meteorology & Atmospheric Sciences
Published
2021

2. Thank You to Our 2018 Peer Reviewers

Author

Rajaram, Harihar, Diffenbaugh, Noah, Camargo, Suzana, Cardenas, M Bayani, Carey, Rebecca, Cobb, Kim, Cory, Rose, Cronin, Meghan, Dombard, Andrew, Donohue, Kathleen, Flesch, Lucy, Giannini, Alessandra, Hayes, Gavin, Hogg, Andrew, Ilyina, Tatiana, Ivanov, Valeriy, Jacobsen, Steven, Korte, Monika, Lu, Gang, Morlighem, Mathieu, Magnusdottir, Gudrun, Newman, Andrew, Opher, Merav, Passalacqua, Paola, Patricola, Christina, Ritsema, Jeroen, Sprintall, Janet, Su, Hui, Thornton, Joel, Williams, Paul, and Yau, Andrew

Subjects
Language, Communication and Culture, Creative and Professional Writing, Creative Arts and Writing, editorial, reviewers, Meteorology & Atmospheric Sciences
Abstract

On behalf of the journal, AGU, and the scientific community, the Editors would like to sincerely thank those who reviewed manuscripts for Geophysical Research Letters in 2018. The hours reading and commenting on manuscripts not only improves the manuscripts but also increases the scientific rigor of future research in the field. We particularly appreciate the timely reviews, in light of the demands imposed by the rapid review process at Geophysical Research Letters. With the revival of the “major revisions” decisions, we appreciate the reviewers' efforts on multiple versions of some manuscripts. Many of those listed below went beyond and reviewed three or more manuscripts for our journal, and those are indicated in italics. In total, 4,484 referees contributed to 7,557 individual reviews in journal. Thank you again. We look forward to the coming year of exciting advances in the field and communicating those advances to our community and to the broader public.

Published
2019

6. Measuring CO[subscript 2]

Author

Taterka, Bruce and Cory, Rose M.

Abstract

This article presents simple tools and concepts to engage students in inquiry-based learning about the carbon cycle, thawing permafrost, and climate change. The lessons focus on learning in Earth science, environmental science, chemistry, and biology and align with the "Next Generation Science Standards".

Published
2016
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7. Ozone depletion, ultraviolet radiation, climate change and prospects for a sustainable future

Author

Barnes, Paul W., Williamson, Craig E., Lucas, Robyn M., Robinson, Sharon A., Madronich, Sasha, Paul, Nigel D., Bornman, Janet F., Bais, Alkiviadis F., Sulzberger, Barbara, Wilson, Stephen R., Andrady, Anthony L., McKenzie, Richard L., Neale, Patrick J., Austin, Amy T., Bernhard, Germar H., Solomon, Keith R., Neale, Rachel E., Young, Paul J., Norval, Mary, Rhodes, Lesley E., Hylander, Samuel, Rose, Kevin C., Longstreth, Janice, Aucamp, Pieter J., Ballaré, Carlos L., Cory, Rose M., Flint, Stephan D., de Gruijl, Frank R., Häder, Donat-P., Heikkilä, Anu M., Jansen, Marcel A. K., Pandey, Krishna K., Robson, T. Matthew, Sinclair, Craig A., Wängberg, Sten-Åke, Worrest, Robert C., Yazar, Seyhan, Young, Antony R., and Zepp, Richard G.

Published
2019
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16. Thank You to Our 2021 Peer Reviewers

Author

Rajaram, Harihar, primary, Camargo, Suzana, additional, Cappa, Christopher D., additional, Carey, Rebecca, additional, Cory, Rose M., additional, Dombard, Andrew J., additional, Donohue, Kathleen A., additional, Flesch, Lucy, additional, Giannini, Alessandra, additional, Gu, Yu, additional, Huber, Christian, additional, Ivanov, Valeriy, additional, Korte, Monika, additional, Lu, Gang, additional, Morlighem, Mathieu, additional, Magnusdottir, Gudrun, additional, Opher, Merav, additional, Patricola, Christina M., additional, Prieto, Germán A., additional, Qiu, Bo, additional, Su, Hui, additional, Sun, Daoyuan, additional, Thornton, Joel A., additional, Wang, Kaicun, additional, Whalen, Caitlin, additional, White, Angelicque E., additional, Williams, Quentin, additional, and Yau, Andrew, additional

Published
2022
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17. Inter‐laboratory differences in the apparent quantum yield for the photochemical production of dissolved inorganic carbon in inland waters and implications for photochemical rate modeling

Author

Koehler, Birgit, primary, Powers, Leanne C., additional, Cory, Rose M., additional, Einarsdóttir, Karólína, additional, Gu, Yufei, additional, Tranvik, Lars J., additional, Vähätalo, Anssi V., additional, Ward, Collin P., additional, and Miller, William L., additional

Published
2022
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40. Direct noninvasive 1H NMR analysis of stream water DOM: Insights into the effects of lyophilization compared with whole water.

Author

Whitty, Stephanie D., Waggoner, Derek C., Cory, Rose M., Kaplan, Louis A., and Hatcher, Patrick G.

Subjects
WATER analysis, DISSOLVED organic matter, CHEMICAL structure, FREEZE-drying, MOLECULAR weights, METHYLENE group
Abstract

NMR spectroscopy is widely used in the field of aquatic biogeochemistry to examine the chemical structure of dissolved organic matter (DOM). Most aquatic DOM analyzed by proton NMR (1H NMR) is concentrated mainly by freeze‐drying prior to analysis to combat low concentrations, frequently <100 μM C, and eliminate interference from water. This study examines stream water with low dissolved organic carbon content by 1H NMR with a direct noninvasive analysis of whole water using a water‐suppression technique. Surface waters, collected from the headwaters of the Rio Tempisquito, Costa Rica, were examined directly, and the spectral characteristics were compared with those of the traditional preanalysis freeze‐drying approach revealing significant differences in the relative intensity of peaks between the whole water and freeze‐dried DOM. The freeze‐dried DOM required less time to obtain quality spectra, but several peaks were missing compared with the spectra of whole water DOM; notably the most dominant peak in the spectrum constituting roughly 10% of the DOM. The stream water DOM showed an increase in the relative intensity of aliphatic methyl and methylene groups and a decrease in carbonyl, carboxyl, and carbohydrate functionalities after freeze‐drying. The results of this study show that freeze‐drying alters the original composition of DOM and thus freeze‐dried DOM may not represent the original DOM. The information gained from whole water analysis of stream water DOM in a noninvasive fashion outweighs the attraction of reduced analysis times for preconcentrated samples, particularly for studies interested in investigating the low molecular weight fraction of DOM. [ABSTRACT FROM AUTHOR]

Published
2021
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45. Appreciation of 2017 GRL Peer Reviewers

Author

Diffenbaugh, Noah, primary, Beal, Lisa, additional, Bayani Cardenas, M., additional, Cobb, Kim, additional, Cory, Rose, additional, Cronin, Meghan, additional, Dombard, Andrew J., additional, Hogg, Andrew, additional, Ilyina, Tatiana, additional, Korte, Monika, additional, Lu, Gang, additional, Magnusdottir, Gudrun, additional, Newman, Andrew V., additional, Opher, Merav, additional, Ritsema, Jeroen, additional, Sprintall, Janet, additional, Stroeve, Julienne, additional, Thornton, Joel A., additional, Williams, Paul D., additional, and Yau, Andrew, additional

Published
2018
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49. Professor emphasizes instruction in real meaning of sacraments

Author

Cory, Rose

Subjects
News, opinion and commentary, Sports and fitness
Abstract

Byline: ROSE CORY ROSE CORYSTAFF WRITER On Sept. 29 in the Gallery, students and members of the community gathered to hear why there should be a revived effort to teach [...]

Published
2017

50. Reviews and syntheses: Effects of permafrost thaw on Arctic aquatic ecosystems

Author

Vonk, Jorien E, Tank, Suzanne E, Bowden, William B, Laurion, Isabelle, Vincent, Warwick F, Alekseychik, Pavel, Amyot, Marc, Billett, Michael, Canario, Joao, Cory, Rose M, Deshpande, Bethany N, Helbig, Manuel, Jammet, Mathilde, Karlsson, Jan, and Larouche, Julia

Abstract

The Arctic is a water-rich region, with freshwater systems covering about 16 % of the northern permafrost landscape. Permafrost thaw creates new freshwater ecosystems, while at the same time modifying the existing lakes, streams, and rivers that are impacted by thaw. Here, we describe the current state of knowledge regarding how permafrost thaw affects lentic (still) and lotic (moving) systems, exploring the effects of both thermokarst (thawing and collapse of ice-rich permafrost) and deepening of the active layer (the surface soil layer that thaws and refreezes each year). Within thermokarst, we further differentiate between the effects of thermokarst in lowland areas vs. that on hillslopes. For almost all of the processes that we explore, the effects of thaw vary regionally, and between lake and stream systems. Much of this regional variation is caused by differences in ground ice content, topography, soil type, and permafrost coverage. Together, these modifying factors determine (i) the degree to which permafrost thaw manifests as thermokarst, (ii) whether thermokarst leads to slumping or the formation of thermokarst lakes, and (iii) the manner in which constituent delivery to freshwater systems is altered by thaw. Differences in thaw-enabled constituent delivery can be considerable, with these modifying factors determining, for example, the balance between delivery of particulate vs. dissolved constituents, and inorganic vs. organic materials. Changes in the composition of thaw-impacted waters, coupled with changes in lake morphology, can strongly affect the physical and optical properties of thermokarst lakes. The ecology of thaw-impacted lakes and streams is also likely to change; these systems have unique microbiological communities, and show differences in respiration, primary production, and food web structure that are largely driven by differences in sediment, dissolved organic matter, and nutrient delivery. The degree to which thaw enables the delivery of dissolved vs. particulate organic matter, coupled with the composition of that organic matter and the morphology and stratification characteristics of recipient systems will play an important role in determining the balance between the release of organic matter as greenhouse gases (CO2and CH4), its burial in sediments, and its loss downstream. The magnitude of thaw impacts on northern aquatic ecosystems is increasing, as is the prevalence of thaw-impacted lakes and streams. There is therefore an urgent need to quantify how permafrost thaw is affecting aquatic ecosystems across diverse Arctic landscapes, and the implications of this change for further climate warming.

Published
2015

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