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Value-added Impact of Geostationary Hyperspectral Infrared Sounders on Local Severe Storm Forecasts——via a Quick Regional OSSE

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Advances in Atmospheric Sciences 2018年第10期35卷 1217-1230页

作者： Zhenglong LI Jun LI Pei WANG Agnes LIM Jinlong LI Timothy J.SCHMIT Robert ATLAS Sid-Ahmed BOUKABARA Ross N.HOFFMAN Cooperative Institute for meteorological Satellite Studies University of Wisconsin-Madison Center for Satellite Applications and Research NOAA atlantic oceanographic and meteorological laboratory OAR/NOAA Center for Satellite Applications and Research NOAA

Accurate atmospheric temperature and moisture information with high temporal/spatial resolutions are two of the key parameters needed in regional numerical weather prediction(NWP) models to reliably predict high-impact weather events such as local severe storms(LSSs). High spectral resolution or hyperspectral infrared(HIR) sounders from geostationary orbit(GEO) provide an unprecedented source of near time-continuous, three-dimensional information on the dynamic and thermodynamic atmospheric fields—an important benefit for nowcasting and NWP-based forecasting. In order to demonstrate the value of GEO HIR sounder radiances on LSS forecasts, a quick regional OSSE(Observing System Simulation Experiment)framework has been developed, including high-resolution nature run generation, synthetic observation simulation and validation, and impact study on LSS forecasts. Results show that, on top of the existing LEO(low earth orbit) sounders, a GEO HIR sounder may provide value-added impact [a reduction of 3.56% in normalized root-mean-square difference(RMSD)] on LSS forecasts due to large spatial coverage and high temporal resolution, even though the data are assimilated every 6 h with a thinning of 60 km. Additionally, more frequent assimilations and smaller thinning distances allow more observations to be assimilated, and may further increase the positive impact from a GEO HIR sounder. On the other hand, with denser and more frequent observations assimilated, it becomes more difficult to handle the spatial error correlation in observations and gravity waves due to the limitations of current assimilation and forecast systems(such as a static background error covariance). The peak reduction of 4.6% in normalized RMSD is found when observations are assimilated every 3 h with a thinning distance of 30 km.

关键词： OSSE hyperspectral sounder high-impact weather

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The correctness to the spuriously simulated semi-annual cycle of the sea surface temperature in the equatorial eastern Pacific

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Science China Earth Sciences 2011年第3期54卷 438-444页

作者： SONG ZhenYa QIAO FangLi WANG ChunZai The First Institute of Oceanography State Oceanic Administration Qingdao 266061 China noaa atlantic oceanographic and meteorological laboratory Miami USA

One of the challenges faced by the climate model of the Community Climate System Model version 3 (CCSM3) is the spuriously simulated semi-annual cycle of the sea surface temperature (SST) in the equatorial eastern Pacific. This model bias has limited the performance of the climate simulation and prediction. Based on the surface wave-circulation coupled theory, an atmosphere-wave-ocean coupled model was developed, which incorporates the MASNUM (key laboratory of Marine Sciences and Numerical Modeling) wave number spectral model into CCSM3. The new coupled atmosphere-wave-ocean model successfully removes the spurious semi-annual cycle simulated by the original CCSM3 and reasonably produces an SST annual cycle with warm and cold phases in April and August, respectively. The correlation between the simulated and observed SST in the equatorial eastern Pacific is improved from 0.66 to 0.93. The ocean surface layer heat budget analysis indicates that the wave-induced vertical mixing is responsible for improving the simulation of the SST seasonal cycle in the equatorial eastern Pacific.

关键词：赤道东太平洋逻辑模拟温度循环海洋表面温度国家重点实验室气候模型海面耦合理论

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Global patterns of phosphorus transformation in relation to latitude,temperature and precipitation

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Pedosphere 2021年第1期31卷 214-220页

作者： Jia-Zhong ZHANG Ocean Chemistry and Ecosystems Division Atlantic Oceanographic and Meteorological LaboratoryNational Oceanic and Atmospheric AdministrationMiami FL 33149USA

Dear Editor,Phosphorus (P) is essential and often a limiting nutrient for biological production on land and in the seas (Elser et al., 2007). The biologically available P to terrestrial and aquatic ecosystems ultimate... 详细信息

关键词： latitude phosphorus transformation

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Modulation of Low-Latitude West Wind on Abnormal Track and Intensity of Tropical Cyclone Nargis (2008) in the Bay of Bengal

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Advances in Atmospheric Sciences 2012年第2期29卷 407-421页

作者：李维维王春在王东晓杨磊邓奕 State Key laboratory of Tropical Oceanography South China Sea Institute of OceanologyChinese Academy of ScienceGuangzhou 510301 NOAA/Atlantic Oceanographic and Meteorological Laboratory MiamiFloridaUSA

Tropical cyclone （TC） Nargis （2008） made landfall in Myanmar on 02 May 2008, bringing a storm surge, major flooding, and resulting in a significant death toll. TC Nargis （2008） displayed abnormal features, including rare eastward motion in its late stage, rapid intensification before landing. Using reanalysis data and a numerical model, we investigated how a low-latitude westerly wind modulated TC Nargis’ （2008） track and provided favorable atmospheric conditions for its rapid intensification. More importantly, we found a possible counterbalance effect of flows from the two hemispheres on the TC track in the Bay of Bengal. Our analysis indicates that a strong westerly wind burst across the Bay of Bengal, resulting in TC Nargis’ （2008） eastward movement after its recurvature. This sudden enhancement of westerly wind was mainly due to the rapidly intensified mid-level cross-equatorial flow. Our results show that a high-pressure system in the Southern Hemisphere induced this strong, mid-level, cross-equatorial flow. During the rapid intensification period of TC Nargis （2008）, this strong and broad westerly wind also transported a large amount of water vapor to TC Nargis （2008）. Sufficient water vapor gave rise to continuously high and increased mid-level relative humidity, which was favorable to TC Nargis’ （2008） intensification. Condensation of water vapor increased the energy supply, which eventuated the intensification of TC Nargis （2008） to a category 4 on the Saffir-Simpson scale.

关键词： TC Nargis （2008） tropical cyclone westerly wind cross-equatorial flow Bay of Bengal

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Modulation of Tropical Cyclogenesis in the Western North Pacific by the Quasi-Biweekly Oscillation

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Advances in Atmospheric Sciences 2016年第12期33卷 1361-1375页

作者： Haikun ZHAO Chunzai WANG Ryuji YOSHIDA Key laboratory of meteorological Disaster Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disaster/Pacific Typhoon Research Center/Earth System Modeling CenterNanjing University of Information Science and TechnologyNanjing 210044China NOAA/Atlantic Oceanographic and Meteorological Laboratory MiamiFL33149USA RIKEN Advanced Institute for Computational Science Kobe650-0047Japan

The quasi-biweekly oscillation （QBWO） is the second most dominant intraseasonal mode over the westem North Pacific （WNP） during boreal summer. In this study, the modulation of WNP tropical cyclogenesis （TCG） by the QBWO and its association with large-scale patterns are investigated. A strong modulation of WNP TCG events by the QBWO is found. More TCG events occur during the QBWO＇s convectively active phase. Based on the genesis potential index （GPI）, we further evaluate the role of environmental factors in affecting WNP TCG. The positive GPI anomalies associated with the QBWO correspond well with TCG counts and locations. A large positive GPI anomaly is spatially correlated with WNP TCG events during a life cycle of the QBWO. The low-level relative vorticity and mid-level relative humidity appear to be two dominant contributors to the QBWO-composited GPI anomalies during the QBWO＇s active phase, followed by the nonlinear and potential intensity terms. These positive contributions to the GPI anomalies are partly offset by the negative contribution from the vertical wind shear. During the QBWO＇s inactive phase, the mid-level relative humidity appears to be the largest contributor, while weak contributions are also made by the nonlinear and low-level relative vorticity terms. Meanwhile, these positive contributions are partly cancelled out by the negative contribution from the potential intensity. The contributions of these environmental factors to the GPI anomalies associated with the QBWO are similar in all five flow patterns--the monsoon shear line, monsoon confluence region, monsoon gyre, easterly wave, and Rossby wave energy dispersion associated with a preexisting TC. Further analyses show that the QBWO strongly modulates the synoptic-scale wave trains （SSWs） over the WNP, with larger amplitude SSWs during the QBWO＇s active phase. This implies a possible enhanced （weakened） relationship between TCG and SSWs during the active （inactive） phase. This study improves our understanding of the modulation of WNP TCG b

关键词： tropical cyclogenesis quasi-biweekly oscillation genesis potential index large-scale patterns western NorthPacific

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Effects of Surface Flux Parameterization on the Numerically Simulated Intensity and Structure of Typhoon Morakot(2009)

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Advances in Atmospheric Sciences 2016年第1期33卷 58-72页

作者： Jie MING Jun A.ZHANG Key laboratory of Mesoscale Severe Weather/MOE and School of Atmospheric Sciences Nanjing UniversityNanjing 210023 Hurricane Research Division Atlantic Oceanographic and Meteorological LaboratoryNational Oceanographic and Atmospheric AdministrationMiamiFLUSA Rosenstiel School of Marine and Atmospheric Science University of Miami MiamiFLUSA

The effects of surface flux parameterizations on tropical cyclone（TC） intensity and structure are investigated using the Advanced Research Weather Research and Forecasting（WRF-ARW） modeling system with high-resolution simulations of Typhoon Morakot（2009）.Numerical experiments are designed to simulate Typhoon Morakot（2009） with different formulations of surface exchange coefficients for enthalpy（C_K） and momentum（C_D） transfers,including those from recent observational studies based on in situ aircraft data collected in atlantic hurricanes.The results show that the simulated intensity and structure are sensitive to C_K and C_D,but the simulated track is not.Consistent with previous studies,the simulated storm intensity is found to be more sensitive to the ratio of C_K/C_D than to C_K or C_D alone.The pressure-wind relationship is also found to be influenced by the exchange coefficients,consistent with recent numerical studies.This paper emphasizes the importance of C_D and C_K on TC structure simulations.The results suggest that C_D and C_K have a large impact on surface wind and flux distributions,boundary layer heights,the warm core,and precipitation.Compared to available observations,the experiment with observed C_D and C_K generally simulated better intensity and structure than the other experiments,especially over the ocean.The reasons for the structural differences among the experiments with different C_D and C_K setups are discussed in the context of TC dynamics and thermodynamics.

关键词： Typhoon Morakot,surface flux parameterization,exchange coefficients,boundary layer

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On the ENSO Mechanisms

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Advances in Atmospheric Sciences 2001年第5期18卷 674-691页

作者： Chunzai Wang Physical Oceanography Division NOAA Atiantic Oceanographic and Meteorological LaboratoryMiamiFloridaU.S.A.

The El Nino-Southern Oscillation (ENSO) is an interannual phenomenon involved in the tropical Paci- fic Ocean-atmosphere interactions. The oscillatory nature of ENSO requires both positive and negative ocean-atmosphere feedbacks. The positive feedback is dated back to Bjerknes' hypothesis in the 1960s, and different negative feedbacks have been proposed since the 1980s associated with the delayed oscillator, the western Pacific oscillator, the recharge-discharge oscillator, and the advective-reflective oscillator. The de- layed oscillator assumes that wave reflection at the western boundary provides a negative feedback for the coupled system to oscillate. The western Pacific oscillator emphasizes equatorial wind in the western Pacific that provides a negative feedback for the coupled system. The recharge-discharge oscillator argues that discharge and recharge of equatorial heat content cause the coupled system to oscillate. The advective-re- flective oscillator emphasizes the importance of zonal advection associated with wave reflection at both the western and eastern boundaries. All of these physics are summarized in a unificd ENSO oscillator. The de- layed oscillator, the western Pacific oscillator, the recharge-discharge oscillator, and the advective-reflec- tive oscillator can be extracted as special cases of the unified oscillator. As suggested by this unified oscillator, all of the previnus ENSO oscillator mechanisms may be operating in nature.

关键词： El Nino-Southern Oscillation Ocean-atmosphere interactions ENSO theory Climate varisbility

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Research advances on internal processes affecting tropical cyclone intensity change from 2018–2022

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Tropical Cyclone Research and Review 2023年第1期12卷 10-29页

作者： Xiaomin Chen Christopher M.Rozoff Robert F.Rogers Kristen L.Corbosiero Dandan Tao Jian-Feng Gu Falko Judt Eric A.Hendricks Yuqing Wang Michael M.Bell Daniel P.Stern Kate D.Musgrave John A.Knaff John Kaplan noaa/OAR/atlantic oceanographic and meteorological laboratory MiamiUSA University of Alabama in Huntsville HuntsvilleUSA National Center for Atmospheric Research BoulderUSA University at Albany/State University of New York AlbanyUSA University of Bergen BergenNorway Nanjing University NanjingChina University of Reading ReadingUK University of Hawaii at Manoa HonoluluUSA Colorado State University Fort CollinsUSA University Corporation for Atmospheric Research MontereyUSA noaa Center for Satellite Applications and Research Fort CollinsUSA Department of Atmospheric and Earth Science University of Alabama in HuntsvilleHuntsvilleUSA

This contribution summarizes the significant progress in a variety of topic areas related to internal tropical cyclone(TC)intensity change processes over 2018–2022 from the WMO Tenth International Workshop on Tropical Cyclones(IWTC-10).These topic areas include surface and boundary layer processes;TC internal structure and microphysical processes;and,radiation interactions with TCs.Recent studies better frame the uncertainty in the surface drag and enthalpy coefficients at high wind speeds.These parameters greatly impact TC intensity and it is therefore important that more direct measurements of these boundary layer parameters are made.Particularly significant scientific strides have been made in TC boundary layers.These advancements have been achieved through improved coupled models,large-eddy simulations,theoretical advance-ments,and detailed observations.It is now clear that the research field needs to better represent the eddy viscosity throughout the depth of the boundary layer.Furthermore,detailed study of coherent structures in TC boundary layers will likely be a propitious direction for the research community.Meanwhile,in-depth observational field campaigns and assiduous data analysis have made significant headway into verifying theory and modeling studies of intensification processes related to TC vortex alignment,efficient latent heating distributions,and overall 3D structure.Substantial efforts have also been made to better understand the intricate roles radiative processes play in TC evolution and intensity change.Finally,some promising progress has been made in the development of time-dependent theories of TC intensification and the predictability of internal TC intensity change.Overall,there have been well-earned gains in the understanding of intensity change processes intrinsic to the TC system,but the journey is not complete.This paper highlights some of the most relevant and important research areas that are still shedding new light into internal factors governing TC intensity change.

关键词： Tropical cyclone Intensity Internal dynamics Boundary-layer processes Observations Predictability

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BEntropy Production of Moving Bed Reactors

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Journal of Iron and Steel Research(International) 1995年第1期2卷 6-9页

作者： YAN Jian Guo CHEH Yung Ting TANG Zhong He NOAA/Atlantic Oceanographic and Meteorological Laboratory Dept.of Physical Chemistry Central Iron and Steel Research Institute

We present an entropy production formulationn for a gas-solid moving bed reactor,which we have not seen in any published reference. Apart from the traditional “flows” and “forces”,e. g., those for heat conduction and mass diffusions in each phase , we introduced the heterogeneouseffects: gas-solid heat and mass transfer, which lead to some new flows and forces in the entropyproduction formulation.

关键词： gas-solid system moving bed reactor entropy production

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Modeling study of a severe aerosol pollution event in December 2013over Shanghai China:An application of chemical data assimilation

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Particuology 2015年第3期13卷 41-51页

作者： Jian-Bin Wu Jianming Xu Mariusz Pagowski Fuhai Geng Songqiang Gu Guangqiang Zhou Ying Xie Zhongqi Yu Shanghai meteorological Service noaa Earth System Research laboratory(ESRL)

This study focuses on the importance of initial conditions to air-quality predictions. We ran assimilation experiments using the WRF-Chem model and grid-point statistical interpolation （GSI）, for a 9-day severe particulate matter pollution event that occurred in Shanghai in December 2013. In this application, GSI used a three-dimensional variational approach to assimilate ground-based PM2.s observations into the chemical model, to obtain initial fields for the aerosol species. In our results, data assimilation significantly reduced the errors when compared to a simulation without assimilation, and improved forecasts of PM2.5 concentrations. Despite a drop in skill directly after the assimilation, a positive effect was present in forecasts for at least 12-2413, and there was a slight improvement in the 48-h forecasts. In addition to performing well in Shanghai, the verification statistics for this assimilation experiment are encouraging for most of the surface stations in China.

关键词： Data assimilationAerosol pollutionInitial conditionForecastingPM2.5

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