scispace - formally typeset
L

Leo van Kampenhout

Researcher at Utrecht University

Publications -  7
Citations -  1108

Leo van Kampenhout is an academic researcher from Utrecht University. The author has contributed to research in topics: Greenland ice sheet & Ice sheet. The author has an hindex of 6, co-authored 7 publications receiving 546 citations.

Papers
More filters
Journal ArticleDOI

The Community Land Model version 5 : description of new features, benchmarking, and impact of forcing uncertainty

David M. Lawrence, +60 more
TL;DR: The Community Land Model (CLM) is the land component of the Community Earth System Model (CESM) and is used in several global and regional modeling systems.
Journal ArticleDOI

Present-day and future Antarctic ice sheet climate and surface mass balance in the Community Earth System Model

TL;DR: In this paper, the authors presented climate and surface mass balance (SMB) of the Antarctic ice sheet (AIS) as simulated by the global, coupled ocean-atmosphere-land Community Earth System Model (CESM) with a horizontal resolution of $${\sim }1^\circ$$
Journal ArticleDOI

Greenland Ice Sheet Surface Mass Loss: Recent Developments in Observation and Modeling

TL;DR: This paper reviewed recent developments in the observation and modeling of GrIS surface mass balance (SMB), published after the July 2012 deadline for the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC AR5).
Journal ArticleDOI

GrSMBMIP: intercomparison of the modelled 1980-2012 surface mass balance over the Greenland Ice Sheet

TL;DR: In this article, the authors compare the performance of different surface mass balance (SMB) models over the Greenland Ice Sheet (GrSMBMIP) for the common period 1980-2012.
Journal ArticleDOI

Representing Greenland ice sheet freshwater fluxes in climate models

TL;DR: In this paper, a long-term (1850-2200) best estimate of Greenland ice sheet (GrIS) freshwater runoff is presented, which improves spatial detail of runoff locations and temporal resolution, and the model results suggest that the decrease in Atlantic Meridional Overturning Circulation (AMOC) is dominated by warming of the surface ocean and enhanced GrIS freshwater forcing leads to a slightly enhanced weakening of the AMOC.