<p>Identification and validation of atmospheric extremes is essential to monitoring climate change, to addressing engineering and safety concerns, and to promoting technological advancement.<a href="http://www.indiaenvironmentportal.org.in/files/file/Megaflash-Lightning-Extremes.pdf"
<p>Equilibrium climate sensitivity, the global surface temperature response to CO$_2$ doubling, has been persistently uncertain. <a href="http://www.indiaenvironmentportal.org.in/files/file/climate-sensitivity.pdf"
<p>Continuous seismic observations across the Ross Ice Shelf reveal ubiquitous ambientresonances at frequencies >5 Hz.<a href="http://www.indiaenvironmentportal.org.in/files/file/Ross_Iceshelf_Chaput_et_al-2018-Geophysical_Research_Letters.pdf"
<p>Hypothesized drawdown of the East Antarctic Ice Sheet through the “bottleneck” zone between East and West Antarctica would have significant impacts for a large proportion of the Antarctic
<p>Rapid intensification (RI) of hurricanes is notoriously difficult to predict and can contribute to severe destruction and loss of life. While past studies examined the frequency of RI occurrence, changes
<p>Lava flow thicknesses, volumes, and effusion rates provide essential information for understanding the behavior of eruptions and their associated deformation signals. Preeruption and posteruption elevation
<p>Many glaciers in the northwest of High Mountain Asia (HMA) show an almost zero or positive mass balance, despite the global trend of melting glaciers. This phenomenon is often referred to as the “Karakoram
<p>By applying an inversion algorithm to NOx satellite observations from Ozone Monitoring Instrument, monthly NOx emissions for a 10 year period (2007 to 2016) over Chinese seas are presented for the first
<p>The causative source of the first damaging earthquake instrumentally recorded in the Island of Ischia, occurred on 21 August 2017, has been studied through a multiparametric geophysical approach. In
<p>Fault behavior during an earthquake is controlled by the state of stress on the fault. Complex coseismic fault slip on large earthquake faults has recently been observed by dense seismic networks, which
