Publications

Submitted
Fernando DN, Fu R, Solis S, Mace RE, Sun Y, Yan B, Pu B. Assessing the potential for providing an early warning of summer drought over Texas and the south central United States. Water Resource Research. Submitted.
2018
Chakraborty S, Schiro KA, Fu R, Neelin JD. On the role of aerosols, humidity, and vertical wind shear in the transition of shallow to deep convection at the Green Ocean Amazon 2014/5 site. Atmospheric Chemistry and Physics Discussions [Internet]. 2018. Publisher's VersionAbstract

The preconditioning of the atmosphere for a shallow-to-deep convective transition during the dry-to-wet season transition period (August–November) is investigated using Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) GoAmazon2014/5 campaign data from March 2014 to November 2015 in Manacapuru, Brazil. In comparison to conditions observed prior to shallow convection, anomalously high humidity in the free troposphere and boundary layer is observed prior to a shallow-to-deep convection transition. An entraining plume model, which captures this leading dependence on lower-tropospheric moisture, is employed to study indirect thermodynamic effects associated with vertical wind shear (VWS) and cloud condensation nuclei (CCN) concentration on pre-convective conditions. The shallow-to-deep convective transition primarily depends on humidity, especially that from the free troposphere, which tends to increase plume buoyancy. Conditions preceding deep convection are associated with high relative humidity, and low-to-moderate CCN concentration (less than the 67th percentile, 1274 cm−3). VWS, on the other hand, shows little relation to moisture and plume buoyancy. Buoyancy estimates suggest that the latent heat release due to freezing is important to deep convective growth under all conditions analyzed, consistent with potential pathways for aerosols effects, even in presence of a strong entrainment. Shallow-only convective growth, on the other hand, shows an association with a strong (weak) low (deep) level VWS and with higher CCN concentration.

Zhuang Y, Fu R, Wang H. How do environmental conditions influence vertical buoyancy structure and shallow-to-deep convection transition across different climate regimes?. Journal of the Atmospheric Sciences [Internet]. 2018;75 (6) :1909-1932. Publisher's VersionAbstract

We developed an entraining parcel approach that partitions parcel buoyancy into contributions from different processes, e.g. adiabatic cooling, condensation, freezing, and entrainment. Applying this method to research quality radiosonde profiles provided by the Atmospheric Radiation Program (ARM) at six sites, we evaluated how atmospheric thermodynamic conditions and entrainment influence various physical processes that determine the vertical buoyancy structure across different climate regimes as represented by these sites. The differences of morning buoyancy profiles between the deep convection/transition cases (DC) and shallow convection/non-transition cases (SC) were used to assess pre-conditions important for shallow-to-deep convection transition. Our results show that for continental sites such as the U.S. Southern Great Plains (SGP) and the West-Central Africa, surface condition alone is enough to account for the buoyancy difference between DC and SC cases, although entrainment further enhances the buoyancy difference at SGP. For oceanic sites in the Tropical West Pacific, humidity dilution in the lower-to-mid free troposphere (~1-6km) and temperature mixing in the mid-to-upper troposphere (>4km) have the most important influences on the buoyancy difference between DC and SC cases. For the humid Central Amazon region, entrainment in both the boundary layer and the lower free troposphere (~0-4km) have significant contributions to the buoyancy difference; the upper tropospheric influence seems unimportant. In addition, the integral of the condensation term, which represents the parcel's ability to transform available water vapor into heat through condensation, provides a better discrimination between DC and SC cases than the integral of buoyancy or the Convective Available Potential Energy (CAPE).

2017
Koster RD, Betts AK, Dirmeyer PA, Bierkens M, Bennett KE, Déry SJ, Evans JP, Fu R, Hernandez F, Leung LR, et al. Hydroclimatic variability and predictability: a survey of recent research. Hydrology and Earth System Sciences [Internet]. 2017;21 :3777-3798. Publisher's Version
Bowerman AR, Fu R, Yin L, Fernando DN, Arias PA, Dickinson RE. An influence of extreme southern hemispheric cold surges on the North Atlantic Subtropical High through a shallow atmospheric circulation. Journal of Geophysical Research: Atmospheres [Internet]. 2017;122. Publisher's Version bowerman_et_al-2017-journal_of_geophysical_research_atmospheres.pdf
Zhao B, Liou KN, Gu Y, Jiang JH, Li QB, Fu R, Huang L, Liu XH, Shi XG, Su H, et al. A water vapor modulated aerosol impact on ice crystal size. Atmospheric Chemistry and Physics Discussion. 2017.
Zhang K, Fu R, Shaikh M, Ghan S, Wang M, Leung LR, Dickinson RE, Marengo J. Influence of Superparameterization and a Higher-Order Turbulence Closure on Rainfall Bias Over Amazonia in Community Atmosphere Model Version 5. Journal of Geophysical Research: Atmospheres [Internet]. 2017;122. Publisher's Version
Marengo JA, Fisch GF, Alves LM, Sousa NV, Fu R, Zhuang Y. Meteorological context of the onset and end of the rainy season in Central Amazonia during the GoAmazon2014/5. Atmospheric Chemistry and Physics [Internet]. 2017;2017 (12) :7671-7681. Publisher's Version marengo_et_al._-_2017_-_meteorological_context_of_the_onset_and_end_of_the_rainy_season_in_central_amazonia_during_the_goamazon201452.pdf
Wright JS, Fu R, Worden JR, Chakraborty S, Clinton NE, Risi C, Sun Y, Yin L. A rainforest initiated wet season onset over the southern Amazon. Proceedings of the National Academy of Sciences. 2017. wright_et_al._-_2017_-_rainforest-initiated_wet_season_onset_over_the_southern_amazon.pdf
Zhuang Y, Fu R, Marengo JA, Wang H. Seasonal variation of shallow-to-deep convection transition and its link to the environmental conditions over the Central Amazon. Journal of Geophysical Research: Atmospheres [Internet]. 2017;122 (5) :2649–2666. Publisher's VersionAbstract

We analyze simulated sea ice changes in eight different Earth System Models that have conducted experiment G1 of the Geoengineering Model Intercomparison Project (GeoMIP). The simulated response of balancing abrupt quadrupling of CO 2 (abrupt4xCO2) with reduced shortwave radiation successfully moderates annually averaged Arctic temperature rise to about 1°C, with modest changes in seasonal sea ice cycle compared with the preindustrial control simulations (piControl). Changes in summer and autumn sea ice extent are spatially correlated with temperature patterns but much less in winter and spring seasons. However, there are changes of ±20% in sea ice concentration in all seasons, and these will induce changes in atmospheric circulation patterns. In summer and autumn, the models consistently simulate less sea ice relative to preindustrial simulations in the Beaufort, Chukchi, East Siberian, and Laptev Seas, and some models show increased sea ice in the Barents/Kara Seas region. Sea ice extent increases in the Greenland Sea, particularly in winter and spring and is to some extent associated with changed sea ice drift. Decreased sea ice cover in winter and spring in the Barents Sea is associated with increased cyclonic activity entering this area under G1. In comparison, the abrupt4xCO2 experiment shows almost total sea ice loss in September and strong correlation with regional temperatures in all seasons consistent with open ocean conditions. The tropospheric circulation displays a Paci fi c North America pattern-like anomaly with negative phase in G1-piControl and positive phase under abrupt4xCO2-piControl.

Zhuang_et_al.-2017.pdf
Alves LM, Marengo JA, Fu R, Bombardi RJ. Sensitivity of Amazon Regional Climate to Deforestation. American Journal of Climate Change [Internet]. 2017;06 (01) :75–98. Publisher's VersionAbstract

It is known that the Amazon region plays an important role in the global energy, hydrological cycle and carbon balance. This region has been suffering from the course of the past 40 years intense land use and land cover changes. With this in mind, this study has examined possible associations between change in spatial and temporal rainfall variability and land cover change in the Amazon, using the PRECIS regional modelling system. It has been found that the impacts of land cover change by forest removal are more intense in the so-called “Arc of deforestation” over central and southern Amazonia. However, the relative impact of the simulated rainfall changes seems to be more important in the JJA dry season. In addition, the simulations under the deforestation scenarios also show the occurrence of extreme rainfall events as well as more frequent dry periods. Therefore, the results found show to be potentially important in the modulation of regional climate variations which have several environmental and socio-economic impacts.

alves_et_al._-_2017_-_sensitivity_of_amazon_regional_climate_to_deforestation.pdf
2016
Gao HL, Zhang S, Fu R, Li WH, Dickinson RE. Interannual Variation of the Surface Temperature of Tropical Forests from Satellite Observations. Advances in Meteorology [Internet]. 2016;2016 :1-11. Publisher's Version
Pu B, Dickinson RE, Fu R. Dynamical connection between Great Plains low-level winds and variability of central Gulf States precipitation. Journal of Geophysical Research: Atmospheres [Internet]. 2016;121 (7) :3421–3434. Publisher's Version
Zhang K, Fu R, Wang T, Liu Y. Impact of geographic variations of convective and dehydration center on stratospheric water vapor over the Asian monsoon region. Atmospheric Chemistry and Physics Discussions [Internet]. 2016 :1–19. Publisher's VersionAbstract
The Asian monsoon region is the most prominent moisture center of lower stratospheric (LS) water vapor during boreal summer. Previous studies have suggested that the transport of water vapor to the Asian monsoon LS is controlled by dehydration temperatures and convection mainly over the Bay of Bengal and Southeast Asia. However, there is a clear geographic variation of convection associated with the seasonal and intra-seasonal variations of the Asian monsoon circulation, and the relative influence of such a geographic variation of convection vs. the variation of local dehydration temperatures on water vapor transport is still not clear. Using the Aura Microwave Limb Sounder (MLS) satellite observations and a domain-filling forward trajectory model, we show that almost half of the seasonal water vapor increase in the Asian monsoon LS are attributable to the geographic variations of convection and resultant variations of dehydration center, comparable to the influence of the local dehydration temperature increase. In particular, dehydration temperatures are coldest over the southeast and warmest over the northwest within the Asian monsoon region. Although convective center is located over the southeastern Asia, an anomalous increase of convection over the northwestern Asian monsoon region increases the local diabatic heating in the tropopause layer and air mass entering the LS that is dehydrated at relatively warm er temperatures. The warmer dehydration temperatures allow anomalously moist air enters the LS and then moves eastward along the northern frank of the monsoon anticyclonic flow, leading to wet anomalies in the LS over the Asian monsoon region. Likewise, when convection increases over the southeastern Asian monsoon region, dry anomalies appear in the LS. On seasonal scale, this feature is associated with the march of the monsoon circulation, convection and diabatic heating towards the northwestern Asia monsoon from June to August, leading to an increasing fraction of the air mass to be dehydrated at warmer temperatures over the nort hwestern Asian monsoon region. Work presented here confirms the dominant role of temper atures and also emphasizes that one should take the geographic variations of dehydration center into consideration when studying water vapor variations in the LS, as it is linked to changes of convection and large-scale circulation.
Chakraborty S, Fu R, Massie ST, Stephens G. Relative influence of meteorological conditions and aerosols on the lifetime of mesoscale convective systems. Proceedings of the National Academy of Sciences [Internet]. 2016;113 (27) :7426–7431. Publisher's VersionAbstract
Using collocated measurements from geostationary and polar-orbital satellites over tropical continents, we provide a large-scale statistical assessment of the relative influence of aerosols and meteorological conditions on the lifetime of mesoscale convective systems (MCSs). Our results show that MCSs' lifetime increases by 3–24 h when ver-tical wind shear (VWS) and convective available potential energy (CAPE) are moderate to high and ambient aerosol optical depth (AOD) increases by 1 SD (1$\sigma$). However, this influence is not as strong as that of CAPE, relative humidity, and VWS, which increase MCSs' lifetime by 3–30 h, 3–27 h, and 3–30 h per 1$\sigma$ of these variables and explain up to 36%, 45%, and 34%, respectively, of the variance of the MCSs' lifetime. AOD explains up to 24% of the total variance of MCSs' lifetime during the decay phase. This result is physically con-sistent with that of the variation of the MCSs' ice water content (IWC) with aerosols, which accounts for 35% and 27% of the total variance of the IWC in convective cores and anvil, respectively, dur-ing the decay phase. The effect of aerosols on MCSs' lifetime varies between different continents. AOD appears to explain up to 20–22% of the total variance of MCSs' lifetime over equatorial South America compared with 8% over equatorial Africa. Aerosols over the Indian Ocean can explain 20% of total variance of MCSs' lifetime over South Asia because such MCSs form and develop over the ocean. These regional differences of aerosol impacts may be linked to different meteorological conditions. mesoscale convective systems | aerosols | meteorological parameters T he hypothesis that aerosols may delay precipitation and increase cloud lifetime of shallow marine clouds (1) has motivated many researchers to study the aerosol indirect effect on convective clouds; however, the influence of aerosols on enhancing cloud lifetime has remained under debate. Mesoscale convective systems (MCSs) are deep convective clouds that cover several hundred kilometers. Previous studies have shown that aerosols affect deep convection, in particular that aerosols increase the number of smaller size cloud condensation nuclei (CCN) (2), which weaken coagulation and coalescence that form rain droplets, and consequently delay warm rainfall (3, 4). These processes allow more cloud droplets to rise above the freezing level and increase latent heat released due to glaciation (5), resulting in stronger updraft speed, enhanced cloud ice content (6), larger anvil size (5), and higher cloud top height (7). The top of the troposphere warms owing to the aerosol-induced changes in convective anvils (8). Although these aerosol effects have been seen in observations from field cam-paigns (9, 10), they have been undetectable on large spatial and multiyear scales. Rosenfeld et al. (11) have attributed this lack of detectability on the large scale of aerosol invigoration of convec-tion to its variation with meteorological conditions and to the lack of knowledge of the relative humidity (RH) outside the clouds. The variation of aerosol effects on convection with meteoro-logical parameters has been studied previously (11). For example, model simulation has shown that an increase in aerosol concen-trations up to an optimal level can invigorate the MCSs under weak vertical wind shear (VWS) and higher RH but suppress the MCSs under strong VWS in a dry environment (12, 13). They found that, due to a significant enhancement in the convective available po-tential energy (CAPE), corresponding to an increase in RH from 50% to 70%, aerosol impact on ice crystal mass becomes pro-nounced, with a dramatic increase in the size of the anvils and the mass of ice crystals of the deep convection. However, such impacts are negligible when RH increases from 40% to 50%, due to little increase in CAPE (13). Moreover, consumption of CAPE for a given amount of rainfall is converted to an equal amount of kinetic energy that invigorates the convection (5, 14). These studies indicate that VWS, RH, and CAPE are important factors that can influence aerosol impacts on the MCSs. However, no quantitative assessment of the relative influence of aerosols versus these meteorological parameters on convective lifetime using satellite measurements has been established (11). The influence of aerosols on the MCSs is expected to vary in different phases of the convective life cycle. For example, Rosenfeld et al. (5) hypothesized that the impact of aerosol on deep convec-tion is stronger and more prominent during the dissipating phase. Using cloud-resolving simulations, Fan et al. (15) found out that aerosol microphysical effects intensify the deep convection during the mature and decaying phases by forming a larger number of smaller and long-lasting particles, whereas additional latent heat released due to aerosols' thermodynamic effect is responsible for invigorating the deep convections during the growing phase. Hence, the detection of aerosol impacts might not be visible until the mature phase, as no satellite can directly measure the thermo-dynamic properties.
Fernando DN, Mo KC, Fu R, Pu B, Bowerman A, Scanlon BR, Solis RS, Yin L, Mace RE, Mioduszewski JR, et al. What caused the spring intensification and winter demise of the 2011 drought over Texas?. Climate Dynamics [Internet]. 2016;47 (9-10) :3077–3090. Publisher's Version
Pu B, Fu R, Dickinson RE, Fernando DN. Why do summer droughts in the Southern Great Plains occur in some La Niña years but not others?. Journal of Geophysical Research: Atmospheres [Internet]. 2016;121 (3) :1120–1137. Publisher's Version
2015
Sun Y, Fu R, Dickinson R, Joiner J, Frankenberg C, Gu L, Xia Y, Fernando N. Drought onset mechanisms revealed by satellite solar-induced chlorophyll fluorescence: Insights from two contrasting extreme events. Journal of Geophysical Research: Biogeosciences [Internet]. 2015;120 (11) :2427–2440. Publisher's VersionAbstract
This study uses the droughts of 2011 in Texas and 2012 over the central Great Plains as case studies to explore the potential of satellite-observed solar-induced chlorophyll fluorescence (SIF) for monitoring drought dynamics.We find that the spatial patterns of negative SIF anomalies from the Global Ozone Monitoring Experiment 2 (GOME-2) closely resembled drought intensity maps from the U.S. DroughtMonitor for both events. The drought-induced suppression of SIF occurred throughout 2011 but was exacerbated in summer in the Texas drought. This event was characterized by a persistent depletion of root zone soil moisture caused by yearlong below-normal precipitation. In contrast, for the central Great Plains drought, warmer temperatures and relatively normal precipitation boosted SIF in the spring of 2012; however, a sudden drop in precipitation coupled with unusually high temperatures rapidly depleted soil moisture through evapotranspiration, leading to a rapid onset of drought in early summer. Accordingly, SIF reversed from above to below normal. For both regions, the GOME-2 SIF anomalies were significantly correlated with those of root zone soil moisture, indicating that the former can potentially be used as proxy of the latter for monitoring agricultural droughts with different onset mechanisms. Further analyses indicate that the contrasting dynamics of SIF during these two extreme events were caused by changes in both fraction of absorbed photosynthetically active radiation fPAR and fluorescence yield, suggesting that satellite SIF is sensitive to both structural and physiological/biochemical variations of vegetation. We conclude that the emerging satellite SIF has excellent potential for dynamic drought monitoring.
Fu R. Global warming-accelerated drying in the tropics. Proceedings of the National Academy of Sciences [Internet]. 2015;112 (12) :201503231. Publisher's Version
Lin C, Yang K, Huang J, Tang W, Qin J, Niu X, Chen Y, Chen D, Lu N, Fu R. Impacts of wind stilling on solar radiation variability in China. Scientific Reports [Internet]. 2015;5 :15135. Publisher's VersionAbstract
Solar dimming and wind stilling (slowdown) are two outstanding climate changes occurred in China over the last four decades. The wind stilling may have suppressed the dispersion of aerosols and amplified the impact of aerosol emission on solar dimming. However, there is a lack of long-term aerosol monitoring and associated study in China to confirm this hypothesis. Here, long-term meteorological data at weather stations combined with short-term aerosol data were used to assess this hypothesis. It was found that surface solar radiation (SSR) decreased considerably with wind stilling in heavily polluted regions at a daily scale, indicating that wind stilling can considerably amplify the aerosol extinction effect on SSR. A threshold value of 3.5 m/s for wind speed is required to effectively reduce aerosols concentration. From this SSR dependence on wind speed, we further derived proxies to quantify aerosol emission and wind stilling amplification effects on SSR variations at a decadal scale. The results show that aerosol emission accounted for approximately 20% of the typical solar dimming in China, which was amplified by approximately 20% by wind stilling.

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