HelioWebCochin University of Science and Technology, India
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I[Cochin University of Science and Technology, India]
PI["Parent Institutions (0)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (19)"]
CA["Linked Collaborating Authors (5)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Interaction Between Troposphere And Lower Stratosphere Associated With The Passage Of A Tropical Cyclone Over India
- Dilute Rivers and low Sediment Yields in the Western Ghats (Sahyadri): Slow Erosion of a Steep Terrain With High Rainfall
- Water Environment of Kochi - Risk and Impacts Assessment
- Is ash layer of ~ 8 Ma at ODP-758 from Bay of Bengal and Fe-Mn oxide coated pumice from Central Indian Ocean Basin are from same eruption ?
- Environment and Climate Changes during the Holocene: Inferred from Sedimentary Record/Proxies of a Paleodelta Region, Southwest Coast of India
- Influence of SSTs over Nino-3.4 Region on the Indian Summer Monsoon Rainfall
- Temperature Changes in Equatorial Indian Ocean in Association with El Nino
- Coasts under multiple stresses: lessons learned from ARSTISTICC's eight coastal study sites.
- Coherent response of the Indo-African boreal summer monsoon to Pacific SST captured in Ethiopian rain δ<SUP>18</SUP>O
- Decline in Low Latitudinal Cyclones over North Indian Ocean and its Association with Equatorial Westerlies
- Structural Transformation of the Monsoon Low Level Jetstream on its Passage over the South Asian Region
- Factors Behind the Variability of Cirrus Clouds over the Asian Summer Monsoon Region
- Dynamics of Diurnal Variability of Chlorophyll in the Southern Bay of Bengal
- ENSO modulates the frequency of low-latitudinal tropical cyclones over the Bay of Bengal
- Genesis and trends in marine heatwaves over the tropical Indian Ocean and their interaction with the Indian summer monsoon
- Role of ocean mixed layer depth on Eastward propagation of Madden Julian Oscillation
- Thermodynamic Structure of Atmospheric Boundary Layer over the West Coast of India During the Southwest Monsoon
- Validation of the ESA Aeolus Winds in the Troposphere and Lower Stratosphere Using Atmospheric Radars in Arctic Sweden and in Antarctica
- Hunga Tonga volcanic eruption triggered meteotsunami in the north Indian Ocean.