Rain on Snow Effects of Snow Melt on Flooding in Western Washington
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Global Climate Influencer – Madden Julian Oscillation
MADDEN-JULIAN OSCILLATION GLOBAL CLIMATE INFLUENCER By James Rohman | February 2014 May 17, 2013 October 24, 2013 Figure 1. Following heavy rainfall influenced by the Madden-Julian Oscillation, Typhoon Nari caused substantial flooding along the Mekong and Tonlé Sap Rivers in Cambodia. The flood affected more than 500,000 people, and 300,000 hectares of rice fields were destroyed. The capital city of Phnom Penh (with a population 2.2 million) is marked in the image. Global Climate Influencer | Madden-Julian Oscillation 1 1 IntroductionIntroduction The Madden-Julian Oscillation (MJO) is a slow-moving atmospheric The Madden-Julian Oscillation (MJO) is a slow-moving atmospheric pattern that impacts global tropical and sub-tropical weather. pattern that impacts global tropical and sub-tropical weather. The phenomenon was discovered by Roland Madden and Paul Julian in The phenomenon was discovered by Roland Madden and Paul Julian in 1971. They used ten years of pressure records from Kanton Island and 1971. They used ten years of pressure records from Kanton Island and Singapore to identify a 40-50 day oscillation of zonal wind anomalies in Singapore to identify a 40-50 day oscillation of zonal wind anomalies in the tropical Pacific. the tropical Pacific. Since then, MJO’s recurring pattern of intense rain and thunderstorms Since then, MJO’s recurring pattern of intense rain and thunderstorms followed by an unseasonably dry phase has been identified as occurring followed by an unseasonably dry phase has been identified as occurring every 30-60 days. every 30-60 days. MJO starts in the Indian Ocean as a band of low pressure caused by the MJO starts in the Indian Ocean as a band of low pressure caused by the Indian Ocean Dipole (IOD). -
Atmospheric River Landfall-Latitude Changes in Future Climate Simulations
PUBLICATIONS Geophysical Research Letters RESEARCH LETTER Atmospheric river landfall-latitude changes 10.1002/2016GL070470 in future climate simulations Key Points: Christine A. Shields1 and Jeffrey T. Kiehl1 • Hdeg CCSM4 projects more landfalling winter ARs for Southern 1National Center for Atmospheric Research, Boulder, Colorado, USA California for RCP8.5 scenario due to influences from the subtropical jet • Landfall changes in ARs affecting UK are projected to be seasonally Abstract The latitude of landfall for atmospheric rivers (ARs) is examined in the fully coupled half-degree dependent and influenced primarily version of the Community Climate System Model, version 4 (CCSM4) for warm future climate simulations. by eddy-driven jets fi • Causality of future changes to AR Two regions are examined: U.S. West Coast/North Paci c ARs and United Kingdom/North Atlantic ARs. landfall location differs dynamically Changes in AR landfall-latitude reflect changes in the atmospheric steering flow. West Coast U.S. ARs are between Pacific and Atlantic ARs projected to push equatorward in response to the subtropical jet climate change. UK AR response is dominated by eddy-driven jets and is seasonally dependent. UK simulated AR response is modest in the winter with the largest relative changes occurring in the seasonal transition months. Precipitation associated Correspondence to: with ARs is also projected to increase in intensity under global warming. CCSM4 projects a marked shift to C. A. Shields, higher rainfall rates for Southern California. Small to modest rainfall rates may increase for all UK latitudes, for [email protected] the Pacific Northwest, and central and northern California. Citation: Shields, C. -
Southern Hemisphere Mid- and High-Latitudinal AOD, CO, NO2, And
Ahn et al. Progress in Earth and Planetary Science (2019) 6:34 Progress in Earth and https://doi.org/10.1186/s40645-019-0277-y Planetary Science RESEARCH ARTICLE Open Access Southern Hemisphere mid- and high- latitudinal AOD, CO, NO2, and HCHO: spatiotemporal patterns revealed by satellite observations Dha Hyun Ahn1, Taejin Choi2, Jhoon Kim1, Sang Seo Park3, Yun Gon Lee4, Seong-Joong Kim2 and Ja-Ho Koo1* Abstract To assess air pollution emitted in Southern Hemisphere mid-latitudes and transported to Antarctica, we investigate the climatological mean and temporal trends in aerosol optical depth (AOD), carbon monoxide (CO), nitrogen dioxide (NO2), and formaldehyde (HCHO) columns using satellite observations. Generally, all these measurements exhibit sharp peaks over and near the three nearby inhabited continents: South America, Africa, and Australia. This pattern indicates the large emission effect of anthropogenic activities and biomass burning processes. High AOD is also found over the Southern Atlantic Ocean, probably because of the sea salt production driven by strong winds. Since the pristine Antarctic atmosphere can be polluted by transport of air pollutants from the mid-latitudes, we analyze the 10-day back trajectories that arrive at Antarctic ground stations in consideration of the spatial distribution of mid-latitudinal AOD, CO, NO2, and HCHO. We find that the influence of mid-latitudinal emission differs across Antarctic regions: western Antarctic regions show relatively more back trajectories from the mid-latitudes, while the eastern Antarctic regions do not show large intrusions of mid-latitudinal air masses. Finally, we estimate the long-term trends in AOD, CO, NO2, and HCHO during the past decade (2005–2016). -
Read Book Pineapple Express : Fun, Colorful Recipes
PINEAPPLE EXPRESS : FUN, COLORFUL RECIPES FROM HAWAII - AMAZING PINEAPPLE RECIPES FOR A FRUITFUL LIFE PDF, EPUB, EBOOK Susan Gray | 82 pages | 14 Oct 2020 | Independently Published | 9798697620229 | English | none Pineapple Express : Fun, Colorful Recipes from Hawaii - Amazing Pineapple Recipes for A Fruitful Life PDF Book Free Return Exchange or money back guarantee for all orders Learn more. Annie books friends. Flagging a list will send it to the Goodreads Customer Care team for review. In the s, Old Tom gin, a style with quite a bit more sweetness than London dry, was just beginning to gain popularity in America. Tags: exotic, pineapple, colorful, tropical, summer, pineapple pattern, yellow, green, fresh, pineapple, pineapple, pineapple express, happiness, philippines, cheer, pulp, juice. By Darra Goldstein. How To Stop Emotional Eating. The Double-Decker River hits These are easier than open tarts because the jam doesn't dry out during baking. Blend almond milk, strawberry and pineapple for a smoothie that's so easy you can make it on busy mornings. No matter the time of year, I love taking advantage seasonal fresh fruit when serving signature cocktails at my clients' weddings. By James J. Easy steps to make bite-size pastries topped with pineapple jam. Pineapple Pork Fried Rice. Tropical Overnight Oats Rating: Unrated. Andrea Fazzari. Tags: pineapple, express, pattern, fruit. For over a week California was hit by record-breaking storm after storm. Searching for alcoholic drink recipes? The salsa also works well with chicken and pork. Tags: james franco, comedy, funny, pineapple express, comedy central, roast, this is the end, freaks and geeks, hot, actor, the interview, pop culture. -
Meteorological Conditions Associated with Rain-Related Periglacial Debris Flows on Mount Hood, Oregon and Mount Rainier, Washington
AN ABSTRACT OF THE THESIS OF Lauren E. Parker for the degree of Master of Science in Geography presented on June 10, 2009. Title: Meteorological Conditions Associated with Rain-Related Periglacial Debris Flows on Mount Hood, Oregon and Mount Rainier, Washington Abstract approved: _____________________________________________ Anne W. Nolin In November of 2006 an intense rainstorm of tropical origin, known colloquially as the “Pineapple Express,” inundated the Pacific Northwest region of the United States, initiating numerous periglacial debris flows on several of the stratovolcanoes in the Cascade Range of Oregon and Washington. These debris flows rapidly aggrade channels, deposit thick sediments in their path, and severely damage infrastructure. Consequently, this work seeks to understand the potential meteorological triggering mechanisms of these flow events. Here we focus on Mount Hood, Oregon and Mount Rainier, Washington in the investigation of the meteorological conditions associated with rain-related periglacial debris flow events and the variability of these conditions over time. The objectives of this research are to assess the correlation between “Pineapple Express” and “Atmospheric River” events and rain-related debris flows, and to explore the meteorological conditions associated with debris flow events based on 5 parameters: storm track based on geostrophic flow patterns, temperature, precipitation and orographic enhancement, integrated atmospheric moisture transport, and antecedent snow water equivalent (SWE). Dates for the debris flow events for each mountain were linked with corresponding Pineapple Express circulation and Atmospheric River events. Analysis from this work suggests that there is not a strong correlation between the occurrence of debris flows and the occurrence of Pineapple Express or Atmospheric River events as they are presently defined in the literature. -
December 1-4 2007 Meteorological Analysis
December 1-4 2007 Meteorological Analysis By Greg Sinnett DNR Chief Meteorologist December 2007 Storm Event The December 1-3 storms offered nearly every winter season hazard … •Snow •Strong Winds •Heavy Rainfall •Major Flooding •Landslides •Avalanches •High Coastal Surf •Coastal Flooding NWS Seattle, Washington 19 December 2007. 4 pm Sun Very cold Dec 2 Arctic Air Dam Since Friday… Snow and or mixed L Snow and Rain … Variable Snow Amounts 10 pm Sun Dec 2 L 4 am Mon Dec 3 L 10 am Mon Dec 3 L 4 pm Mon Dec 3 24 hours L 10 pm Mon Dec 3 L 4 am Tue Dec 4 L 10 am Tue Dec 4 L 4 pm Tue Dec 4 48 hours L 4 pm Sun Dec 2 Washington L Hawaii Pineapple Express 10 pm Sun Dec 2 Washington L Hawaii Pineapple Express 4 am Mon Dec 3 Washington L Hawaii Pineapple Express 4 pm Mon Dec 3 24 Hr Washington L Hawaii Pineapple Express 10 pm Mon Dec 3 Washington L Hawaii Pineapple Express 1 am Tue Dec 4 Washington L Hawaii Pineapple Express 4 am Tue Dec 4 Washington L Hawaii Pineapple Express 10 am Tue Dec 4 Washington L Hawaii Pineapple Express 4 pm Tue Dec 4 48 Hours Washington L Hawaii Pineapple Express Mauna Kea Weather Center Katrina Storm was an Extra Tropical Cyclone NOT A Hurricane Seattle Radar Estimated Precipitation 9pm Friday thru 2pm Tuesday Radar Blocked 89 hours Portland Radar Estimated Radar Blocked Precipitation 11pm Friday thru 2pm Tuesday 87 hours 4 pm Sun Dec 2 Surface Wind Speeds 60 mph 10 pm Sun Dec 2 Surface Wind Speeds 60 mph 4 am Mon Dec 3 Surface Wind Speeds 60 mph 10 am Mon Dec 3 Winds Along the Beach… 70mph… Gusts to 84+ mph 60 mph 4 pm -
Extreme Weather Events
Extreme weather events Introduction The further a particular weather event lies from the typical range of that type of event, the more it is likely to be described as an extreme event, irrespective of whether it concerns a violent storm, unusual temperatures, heavy precipitation, drought or flood. 2012 seems to have been a year of extreme weather events (‘superstorm’ Sandy in the USA, high rainfall and floods in the UK, etc.). Other years in the last decade have also contained droughts and wildfires (in the USA and Australia), hurricane Katrina (USA), floods (Pakistan) and heat waves (Russia and France). At the same time it is becoming increasingly accepted that human activity, principally the burning of fossil fuels, is changing the global climate and causing the atmosphere to warm. The average global temperature of the lowermost atmosphere has increased markedly since about 1980. Are the two observations, which operate on different timescales1, connected? Are extreme weather events really becoming more common and/or more severe, or are they perhaps part of the climate’s natural variability? The aim of this document is to investigate these two questions. Some basic physics of a warmer atmosphere As air warms its humidity is able to rise and so the atmosphere carries more water vapour. For example, the water content of the atmosphere increases by 7% for each degree Centigrade rise in temperature, although globally precipitation is expected to rise by only about 2%/°C because relative humidity is typically not expected to change on the global scale.8 1 climate change is defined as changes occurring at least over a few decades whereas extreme weather typically lasts from days to months. -
Atmospheric Rivers: Harbors for Extreme Winter Precipitation by Zack Guido
3 | Feature Article Atmospheric Rivers: Harbors for Extreme Winter Precipitation By Zack Guido ierce winds loaded with moisture Fblasted into the Southwest on Decem- ber 18, 2010, dumping record-setting rain and snow from Southern California to southern Colorado. Fourteen inches of rain drenched St. George, Utah, over six days, while 6 inches soaked parts of northwest Arizona in a torrent that sin- gle-handedly postponed drought. Behind this wet weather was a phe- nomenon called atmospheric rivers, a Figure 1. A satellite image of an atmospheric river striking the Pacific Northwest on term first coined in 1998. ARs, as they November 7, 2006. This event produced about 25 inches of rain in three days. Warm are known to scientists, often deliver colors in the image represent moist air and cool colors denote dry air. The horizontal extreme precipitation, mostly to the band of red and purple at the bottom of the image is the Intertropical Convergence West Coast, but sometimes inland as Zone (ITCZ), a normally moist area that some of the strongest ARs can tap into, as well, prompting researchers to probe how happened in this case. Photo credit: Marty Ralph. they form and the effects they have in a changing climate. They are products of an unevenly heated through March is the peak season for Earth and form during winter, when the ARs that drench Southern California. ARs have caused nearly all of the largest temperature difference between the trop- floods on record in California, account- ics and the poles is greatest. The most intense ARs can transport an ing for most of the $400 million the state amount of water vapor equal to the flow spends each year to repair flood damage. -
Atmospheric Rivers
Atmospheric Rivers What is an Atmospheric River? Atmospheric rivers are relatively narrow regions in the atmosphere that are responsible for most of the transport of water vapor from the tropics. Atmospheric rivers come in all shapes and sizes but those that contain the largest amounts of water vapor and strongest winds are responsible for extreme rainfall events and floods. This type of hydrologic event can affect the entire west coast of North America. These extreme events can disrupt travel, induce mudslides, and cause damage to life and property. Not all atmospheric rivers are disruptive. Many are weak and provide beneficial rain or high elevation snow that is crucial to the water supply. The image on the left shows an atmospheric river that affected South- east Alaska on 11-08-2014. The atmospheric river is marked by the narrow plume of subtropical moisture evident in the Total Precipitable Water field extending from the central Pacific northeastward through the Gulf of Alaska. Why do Atmospheric Rivers Occur in SE Alaska? Due to its location on the western side of the North American continent, SE Alaska is often the target for powerful ocean storms that form over the western and central Pacific Ocean and move eastward, steered by the prevailing westerly upper level jet stream. These powerful low pressure systems often have strong fronts associated with them. Fronts act like a conduit to channel warm, moist air northward and eastward ahead of the low pressure system in what is called the “warm conveyor belt”. The strongest fronts are also regions of strong winds in the lower portions of the atmosphere. -
A Case Study of Four Atmospheric River Events Over the Pacific West Coast of the United States Isaac Arseneau1, Dr
A Case Study of Four Atmospheric River Events Over the Pacific West Coast of the United States Isaac Arseneau1, Dr. Wendell Nuss2 1Valparaiso University OCE 1659628 Abstract 2Naval Postgraduate School Atmospheric Rivers (AR) are moisture phenomena related to cyclones which bring moisture and large amounts of precipitation to areas of enhanced elevation along coastal areas. These events bring much of the rain received by the state of California, and the past winter many AR events brought much-needed rain to the region. Four different events from the 2016 fall through 2017 spring seasons are examined to better identify the relative roles of long-range moisture transport versus local moisture fluxes in AR events. Cross-sections of areas and times of interest during each event are generated, along with trajectory analyses of each event which will aid in determining the origin of the moisture being moved over land. Both the cross-sections and the trajectory analysis are taken from the CFSR (Climate Forecast System Reanalysis) model. It is expected that the results of these processes will support the findings of Dacre et al. (2015), which show that the moisture anomaly present during AR events is not actually due to moisture transport directly along the AR itself. Rather, the AR is the result of moisture convergence due to a combination of the warm conveyor belt forcing the ascent of moisture over the warm front and the trailing cold front forcing ascent as it closes the gap between itself and the warm front. The importance of this research is first and foremost evident in the California region, as water conservation in naturally dry areas is extremely important to the ever-expanding cities and communities present there and October 13, 2016 January 17, 2016 February 7, 2016 April 5, 2016 require long-term planning. -
Inland Impacts of Atmospheric River and Tropical Cyclone Extremes on Nitrate Transport and Stable Isotope Measurements
Environmental Earth Sciences (2019) 78:36 https://doi.org/10.1007/s12665-018-8018-x THEMATIC ISSUE Inland impacts of atmospheric river and tropical cyclone extremes on nitrate transport and stable isotope measurements A. Husic1 · J. Fox2 · E. Adams2 · J. Backus3 · E. Pollock4 · W. Ford5 · C. Agouridis5 Received: 30 June 2018 / Accepted: 19 December 2018 © Springer-Verlag GmbH Germany, part of Springer Nature 2019 Abstract Atmospheric rivers and tropical cyclones originate in the tropics and can transport high rainfall amounts to inland temper- − ate regions. The purpose of this study was to investigate the response of nitrate (NO3 ) pathways, concentration peaks, and 15 18 2 18 13 stable isotope (δ NNO3, δ ONO3, δ HH2O, δ OH2O, and δ CDIC) measurements to these extreme events. A tropical cyclone and atmospheric river produced the number one and four ranked events in 2017, respectively, at a Kentucky USA watershed characterized by mature karst topography. Hydrologic responses from the two events were different due to rainfall character- istics with the tropical cyclone producing a steeper rising limb of the spring hydrograph and greater runoff generation to the 2 18 surface stream compared to the atmospheric river. Local minima and maxima of specific conductance, δ HH2O, δ OH2O, and 13 − 15 18 δ CDIC coincided with hydrograph peaks for both events. Minima and maxima of NO 3 , δ NNO3, δ ONO3, and temperature lagged behind the hydrograph peak for both events, and the values continued to be impacted by diffuse recharge during − hydrograph recession. Quick-flow pathways accounted for less than 20% of the total NO3 yield, while intermediate (30%) and slow-flow (50%) pathways composed the remaining load. -
Atmospheric Rivers in the Australia-Asian Region: a Bom-CMA
RESEARCH FRONT CSIRO PUBLISHING Journal of Southern Hemisphere Earth Systems Science, 2020, 70, 3–16 https://doi.org/10.1071/ES19025 Atmospheric rivers in the Australia-Asian region: a BoM–CMA collaborative study Chengzhi YeA, Huqiang ZhangB,E, Aurel MoiseB,C and Ruping MoD AHunan Meteorological Service, Changsha, China. BBureau of Meteorology, Melbourne, Vic., Australia. CCentre for Climate Research Singapore, Meteorological Service Singapore, Singapore. DEnvironment and Climate Change Canada, Vancouver, Canada. ECorresponding author. Email: [email protected] Abstract. The name ‘atmospheric river’ (AR) could easily be misinterpreted to mean rivers flowing in the sky. But, ARs actually refer to narrow bands of strong horizontal water vapour transport that are concentrated in the lower troposphere. These bands are called ‘atmospheric rivers’ because the water vapour flux they carry is close to the volume of water carried by big river systems on the ground. ARs can cause heavy rainfall events if some physical mechanisms, such as orographic enhancement, exist to set up the moisture convergence and vertical motions necessary to produce condensation. In recent decades, these significant moisture plumes have attracted increasing attention from scientific communities, especially in North America and western Europe, to further understand the connections between ARs and extreme precipitation events which can trigger severe natural disasters such as floods, mudslides and avalanches. Yet very limited research has been conducted in the Australia-Asian (A-A) region, where the important role of atmospheric moisture transport has long been recognised for its rainfall generation and variations. In this paper, we introduce a collaborative project between the Australian Bureau of Meteorology and China Meteorological Administration, which was set up to explore the detailed AR characteristics of atmospheric moisture transport embedded in the A-A monsoon system.