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• metoffice_loan_2018pdf

  a steam sloop used in the Arctic during the British North Atlantic Telegraph Expedition. handwritten 3 volumes MS 539/1 Meteorological register: HMS Bulldog 22.6.1860 3.9.1860 No 1265 handwritten 1 volume MS 539/2 Meteorological register: HMS Bulldog 4.9.1860 6.11.1860 No 1265:a handwritten 1 volume MS

• ar12_all_v03.compressed.pdf

  : Richard G. Derwent INSCON: Peter Simmonds Terra Modus: Dickon Young Contents 1 Executive Summary ........................................................................................................... 3 2 Introduction

• how-can-we-limit-warming-v4.pdf

  to limit warming to given levels, such as the “well-below 2 °C” goal. However these budgets have a large range, due largely to uncertainty in the response of global temperature to carbon emissions. If the climate is more sensitive to carbon than currently thought, budgets will be lower and vice-versa

• The Earth Affecting Solar Causes Observatory (EASCO)

  • EASCO to measure and characterize CMEs and CIRs Science Payload Instrument Measurement FOV SR TR Magnetic and Doppler Imager (MADI) Photosph. B, V Full disk 2” 90 min White-light Coronagraph (WCOR), HI Coronal images 2.5 – 215 Rs 1-2’ 10, 60 min Inner Coronal Imager at EUV (ICIE) Coronal images 0

• location-based-mpa-2025.pdf

  Location based planning averages Prepared for: Example Location Based Planning Averages Site: Exeter, Postcode EX1 3PB Weather Data from: Latitude 50.7242, Longitude -3.5047 Issued on Monday 2 March at 12:06:50 1-in-10 Year Values (1971-2010) Month Daily Rainfall Total (mm) Days of Rain > 5mm Days

• location-based-mpa-2025pdf

  Location based planning averages Prepared for: Example Location Based Planning Averages Site: Exeter, Postcode EX1 3PB Weather Data from: Latitude 50.7242, Longitude -3.5047 Issued on Monday 2 March at 12:06:50 1-in-10 Year Values (1971-2010) Month Daily Rainfall Total (mm) Days of Rain > 5mm Days

• water_resourcespdf

  Impacts of climate change on river flows and flooding at 1.5°C, 2°C and 4°C global warming Figure 1 - Ranges of river flows changes projected at 1.5°C, 2°C and 4°C global warming Climate change projections We simulated the global climate for the present day and at 1.5°C, 2°C and 4°C global warming

• water_resources.pdf

  Impacts of climate change on river flows and flooding at 1.5°C, 2°C and 4°C global warming Figure 1 - Ranges of river flows changes projected at 1.5°C, 2°C and 4°C global warming Climate change projections We simulated the global climate for the present day and at 1.5°C, 2°C and 4°C global warming

• james_tappin-on_the_importance_of_polarisationpdf

  . Has been shown that exposures ≤10min would still give adequate signal to noise (c.f. HI-2 at 80 min). What does polarization provide? ● ● Depth perception, since the scattering function for polarized brightness is much more peaked towards the Thomson sphere than for total brightness

• james_tappin-on_the_importance_of_polarisation.pdf

  . Has been shown that exposures ≤10min would still give adequate signal to noise (c.f. HI-2 at 80 min). What does polarization provide? ● ● Depth perception, since the scattering function for polarized brightness is much more peaked towards the Thomson sphere than for total brightness